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Contents 


August 31, 1995. 


Editorial. 


A Contribution to the Natural Classification of Lower and Middle 
Cambrian Arthropods: Food Gathering and Feeding Mec hanisms . 
E. L. Bousfield 


The Amphipod Superfamily Pontoporeioidea on the Pacific Coast 
of North America. II. Family Haustoriidae. Genus Eohaustorius 
J. L. Barnard: Systematics and Distrihutional Ecology. 

E. L. Bousfield and Phillip M. Hoover 


The Amphipod Family Pleustidae on the Pacific Coast of North 
America. Part III. Subfamilies Parapleustinae, Dactylopleustinae, 
and Pleusirinae: Systematics and Distributional Ecology. 

E. L. Bousfield and E. A. Hendrycks 


Additions to Amphipacifica Vol. I (4). Eusiridae. Cataloguing data. 


35. 


1 


National Library of Canada 


ISSN No. 1 1 89-9905 





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AMPHIPACIFICA 


JOURNAL OF SYSTEMATIC BIOLOGY 


Volume II, Number 1 
August 31, 1995 


AMPHIPACIFICA, Journal of Systematic Biology (ISSN No. 1 189-9905) is published quarterly by 
Amphipacifica Research Publications, 61 1-548 Dallas Rd., Victoria, B. C., Canada, V8V 1B3. 
Annual subscription rates are $40. US or $50. Canadian funds. 


DEDICATION 


The Journal AMPHIPACIFICA is dedicated to the promotion of systematic biology and 
to the conservation of Earth’s natural resources. 


Cover design: Adapted from the title page of S. J. Holmes (1904). “Amphipod 

Crustaceans of the Expedition.” 

Harriman Alaska Expedition, pages 233-244. 


AMPHIPACIFICA VOL. H NO. 1. AUG. 31, 1995. 

EdISt@iro§ill „ 

Since completion of the first volume of Amphipacifica 
last spring, we have continued to receive expressions of both 
satisfaction and criticism concerning the quality of its content 
and editorial format. The commentary came from a wide 
spectrum of readers including: MarkCostello, Dublin, Ireland; 
Larry Hamblin, Romford, U. K.; Pierre Noel, Universite de 
Paris, France; John Holsinger, Norfolk, VA.; Patricia 
McLaughlin, Anacortes, WA; Valerie MacDonald, West 
Saamch, Charles Low, Victoria, and Cas Lindsey, Vancouver, 
B . C. Jim Lowry, Australian Museum, Sydney, has pointed 
out a problem in one of early phoxocephalid plates that 
requires clarification. Niel Bruce, University of Copenhagen 
Museum, Denmark, has detected a number of editorial 
oversights in previous numbers that we have attempted to 
correct in this issue. Changes include a repositioning of the 
pagination and running head, more restricted use of 
underlining, oversize letters, and boldface type, and reduced 
use of abbreviations in the references. More careful attention 
has been given the alignment of type in parallel columns, and 
to consistency in labeling of illustrations. We welcome your 
further suggestions for improvement. 

As the scope of the journal expands, we encourage 
exchange advertising with other journals of systematic biol- 
ogy, and with societies and agencies concerned with conser- 
vation of natural resources. We welcome submissions of 
medium to large systematic studies, and also shorter research 
papers and review articles that involve some aspect of 
aquatic biology and/or environmental concern. Although 
the journal emphasizes systematic research on aquatic 
invertebrate faunas of the North Pacific, as noted previously, 
publication criteria extend to other biomes (including 
terrestrial), other biotas (including vertebrates and fossil 
animals) and other regions (including the North Atlantic). 

' The first paper of this issue is a contribution to the re- 
classification of arthropods and arthropod-like animals, based 
on feeding and food-gathering mechanisms. Arthropod-like 
fossil animals of the Burgess Shale formation flourished in 
ancient Paleozoic seas some 520 million years ago. As a 
result of later orogenic processes, exquisitely preserved 
fossilized remains of these early crustacean and arachnid- 
like animals can be recovered from Middle Cambrian 
sedimentary rocks now situated at altitudes of about 1.5 km 
a.s.l. This study outlines possible phyletic relationships of 
known fossil species within two major groups of arthropods. 
These are defined as the uniantennates, including the aquatic 
Paleozoic trilobites and modem terrestrial arachnids, and the 
biantennates that encompass the mainly aquatic crustaceans, 
and modem terrestrial myriapod and hexapods. This enorm- 
ous assemblage of joint-legged animals, comprising well 
over one million described species, fossil and recent, has 
been encompassed within a phyletic subdivision of only 9 
superclasses and 29 classes. Quite remarkably, the total 
known Cambrian arthropod fauna of less than 100 fossil 
species, all aquatic, represents 6 of the superclasses and 14 
of the classes, whereas the Recent arthropod fauna of over 


1 

one million described species, both aquatic and terrestrial, is 
contained in only 4 superclasses and 15 classes. Thus, the 
contention of Stephen J. Gould, set forth in his popular book 
"Wonderful Life" (1989), that the Cambrian fauna exhibited 
greater disparity (diversity at high taxonomic level) than at 
any other time in animal evolutionary history, finds strong 
support in the present analysis. 

The second paper in the series treats the sy stematics and 
distributional ecology of North Pacific members of amphipod 
family Haustoriidae. Among macro-cmstaceans, haustoriids 
are one of the most highly modified for a free-burrowing life 
style. The family is most diverse within the western North 
Atlantic region, especially along the sandy estuarine coastline 
of southeastern United States. However, one genus, Eohaust- 
orius, has penetrated the North Pacific and is now nearly 
equally speciose along Asiatic and North American coastlines. 
Its subtidal species occur throughout the Pacfic Rim region. 
However, intertidal species are apparently absent from 
corresponding Asiatic shores. There, winter conditions are 
severe, accompanied by sub- freezing temperature and shore 
icing; in summer, species of the competing fossorial talit- 
roidean family Dogielinotidae dominate intertidally. Along 
corresponding North American Pacific sandy shores, how- 
ever, winter conditions are relatively mild, shore icing is 
lacking and, in summer, only one species of intertidal dogiel- 
inotid occurs, and only along the open coast of Washington 
and Oregon states. Their infaunal densities, ease of collect- 
ing, and sensitivity to inimical substances, render certain 
species of Eohaustorius suitable for bioassay monitoring 
and testing of marine sediment toxicity. 

The final paper is a continuation of a series of revision- 
ary studies on the relatively primitive, benthic, gammaridean 
amphipod family Pleustidae. Member species are mainly 
micro-carnivores and commensals within marine commun- 
ities of sessile invertebrates and attached plants. Subfamilies 
Parapleustinae, Pleusirinae, and Dactylopleustinae, 
investigated here, are almost wholly endemic to the North 
Pacific Brim region. Of the 32 known species combined, all 
but two occur nowhere else. The North Pacific marine shelf 
is characterized by long-term stability of associated biotic 
communities, and equable marine climates. These factors, 
presumably operating throughout the evolutionary devel- 
opment of the three pleustid subfamilies, are considered 
primary in dampening evolutionary thrust in other directions. 

In summary, a remarkable feature of these three papers 
is the coincidental stratigraphic range of the marine animals 
encompassed, from the subtidal to the ocean abyss on the one 
hand, and from the supralittoral zone to high interior mountain 
slopes of British Columbia on the other. 

With respect to the article on Cadborosaurus that ap- 
peared in the special supplementary issue of Amphipacifica, 
Vol. I, commentary pro and con has been received. A few 
excerpts are as follows: "You may have created some 
controversy with "Caddy" but . . you'll have provided some 
foundation for its recognition and study" (Dale Calder letter, 
June 19). "I was most impressed by . . . the paper on 


AMPHIPACIFICA VOL. H NO. 1. AUG. 31, 1995. 2 


AMFEIP ACIFICA: PERSONAE NOVAE. . . 



Cadborosarusu willsi . . . and I should like to distribute it 
among our subscribers (Jon Downes, Centre for Fortean 
Zoology, U. K.). " . . You were right in publishing. Perhaps, 
some day, it might prevent another "Kermode" . . (who 
make) hasty, often erroneous identifications" (Earl Godfrey, 
Ottawa). The popularized version entitled "Cadborosaurus, 
survivor from the deep", Horsdal & Schubart, publishers, 
Victoria, 1 34 pp.. May, 1985, was "read with much interest" 
by several subscribers and friends, including Ian McTaggart 
Cowan, Victoria. Concerning this matter, the resignations of 
dissenting editorial associates of this journal, Craig Staude 
and Phil Lambert, have been accepted, regretfully. We are 
greatly indebted to Craig and Phil for their editorial help with 
previous regular issues of the journal, and wish them well in 
furthering their invertebrate research objectives. 

The authors of the research paper on Cadborosaurus 
did not refer to a paper by Peter Scott and Robert Rines in 
Nature, 258: 466-468, 1975, in which the Loch Ness phe- 
nomenon was newly described as Nessiteras rhombopteryx. 
Their reconstruction, based on fixed demersal strobe flash 


Marianne Wilkinson, B.A. (Eng), Associate Editor, has 
had a varied background in the field of communication and 
education. She has served as a high school teacher, news 
reporter, freelance writer, designer, and photographer. Fol- 
lowing a four-year stint as a humour columnist, she becaame 
publisher and editor-in-chief of British Columbia's "Island 
Life" Magazine. Her avocational interests include writing, 
archeology, paleontology, and the outdoors, and is avid 
about flying. 


Phillip M. Hoover, BSc., majored in biology at the 
University of Victoria, with emphasis on marine pollution 
biology and invertebrate taxonomy. During studies for the 
MSc degree in biology, he served as a teaching and research 
assistant in the laboratory of Dr. Derek V. Ellis with whom 
he co-authored studies on the impact and recovery of marine 
benthos in mine tailing wastes. Phil recently completed stud- 
ies on the systematics of North American Pacific marine 
amphipods of families Haustoriidae, Amphilochidae, and 
Corophiidae, the first of which appears in this issue. 

Production of this issue benefits greatly from the 
experienced editorial services of Tara Steigenberger, former 
assistant editor. Royal British Columbia Museum, Victoria. 


photographs of a partial body, neck and supposed hind 
flipper, portrays a thick-bodied, long-tailed animal with two 
pairs of large flippers. Such is quite unlike Cadborosaurus 
willsi, and the names are thus very probably not synonymous. 
Regretably , the Loch Ness specimen was not "in hand" at any 
time and, in our view, the photographs are not sufficiently 
distinct or complete to form the basis for a reasonably accur- 
ate interpretation of the animal’s external morphology. 

The difficulty of research here cannot be overestimated. 
Acquiring a further large specimen for detailed morphologi- 
cal study is very unlikely, but a small juvenile might again be 
captured alive and its behaviour studied in a marine aquarium. 
Despite several recent sightings in waters of the Saanich pen- 
insula, May - August, 1995, neither video footage nor photo- 
graphic "still" shots of this species at the water surface were 
obtained. However, these new sightings, made independ- 
ently, some by two or more observers simultaneously, in- 
cluding one from a large deep freshwater lake not far from 
Victoria, further support the reality and recurring predict- 
ability of this large, anadromous, vertebrate species. 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 3 


A CONTRIBUTION TO THE NATURAL CLASSIFICATION OF LOWER AND MIDDLE 
CAMBRIAN ARTHROPODS: FOOD-GATHERING AND FEEDING MECHANISMS. 


ABSTRACT 


by E. L. Bousfield, Research Associate 
Royal Ontario Museum, Toronto, Canada MSS 2C6 


The classification of arthropods and arthropodlike invertebrates of Lower and Middle Cambrian strata 
is currently in a state of flux. Reanalysis of these early arthropods, however, indicates that a more widely 
acceptable basis for their natural classification might emphasize mechanisms of food gathering and feeding. 
Moreover, such mechanisms are usually readily determinable in both fossil and living specimens. 

This study employs a relatively broad definition of the term “arthropod”, and utilizes most higher 
classificatory names of the arthropod literature, but with reorganized emphasis. The views of Gould (1989) 
and Briggs et al. (1993) concerning high-level taxonomic diversity (disparity) of Lower and Middle Cambrian 
arthropods ( sensu Walcott, 1912) are generally supported. However, these taxa have all been classified 
previously within accepted arthropod subcategories and none is considered new at the level of phylum or 
subphylum. Although the present analysis suggests plausible evolutionary pathways for food-gathering and 
feeding mechanisms in uniantennate (i.e., chelicerate) lineages, and possibly in biantennate (i.e., crustacean, 
myriapod and hexapod) arthropods, incorporation of these ideas within a suggested formal classification 
awaits broader acceptance among current workers. 


INTRODUCTION 

Arthropods are a major component of a fauna that, dur- 
ing the Cambrian Period, attained what has been described 
by Gould (1989) as a "maximum disparity of animal life". 
This concept, of broad morphological diversity at high tax- 
onomic level (here defined as subclass or higher, or undeter- 
mined), has been questioned in detail by several (e.g., Ridley 
(1990, 1993; Briggs et al. (1992), but ably defended by 
Gould (1993) and Foot & Gould (1992). Thus, disparity of 
arthropods and arthropod-like forms does not appear to have 
been greater in Cambrian than in Recent times, whatever 
classifications are consulted or methodologies used (Wills et 
al., 1994). However, in proportion to the small number 
(< 1 00) of Cambrian arthropod species recorded to date, from 
a half dozen or so major fossil sites world- wide, the percent- 
age of high-level taxa that they represent is very much higher 
than that of comparable samples of Recent faunas. If 
considerations are restricted to aquatic faunas only, the 
percentage difference is even higher. Whatever the magni- 
tude of these differences, however, the Cambrian Period can 
fairly be viewed as ^ period of arthropod evolutionary 
"explosion". 

Cambrian arthropods are mostly unlike living repre- 
sentatives of the phylum, and therefore difficult to classify 
on existing natural bases. One of the richest arthropod as- 
semblages, of about 35 species, has been described from 
Middle Cambrian Burgess Shale deposits in Yoho National 
Park, British Columbia (Conway Morris & Whittington, 
1985). General and popularized treatments of that fauna, by 
Gould (1989) and Briggs et al. (1993), have summarized the 
original work of Charles Walcott (1912), and the subsequent 
careful descriptive treatments by Whittington (1971, 1975), 
Bruton (1981), Briggs (1979, 1981); Briggs & Whittington 
(1983, 1987), Collins (1987a, b), Collins & Rudkin (1981), 
Conway Morris (1986) and others. Their work has made 


possible the present re-analysis of the etaly arthropod fauna 
for which the author feels most grateful. 

Previous work has revealed a plethora of Cambrian tax- 
onomic oddities several of which, according to Gould (1989), 
may require new higher classification, even at the level of 
phylum. Gould accepted, justifiably, the morphological 
interpretations of the aforementioned principal workers in 
this unfolding paleontological drama. Recent field work, 
especially in the Chengjiang region of southern China (Hou 
et al . 1991), and in Greenland (Conway Morris et al . 1987), 
has yielded many more important new taxa (e.g., by Hou, 1987 
a, b; Hou & Bergstrom, 1991; Chen, etal. 1994). During his 
relatively brief two-year book-compilation period, Gould 
(1989) touched on the initial papers by Hou; however, he did 
not reference other pertinent works of group specialists (e.g. 
of Bergstrom, 1986; Schram, 1986; Dahl, 1984, 1987) that 
embody alternative and possibly more plausible classifica- 
tions and evolutionary starting points, as suggested by the 
writer (Bousfield, 1987), for some of the major Burgess 
arthropod groups. Some reviewers (e.g., Fortey, 1989) have 
pointed to papers on cladistic classificatory methodology 
(e.g., Briggs & Fortey, 1989) that do provide credible, but not 
entirely correct, classifications of some of the enigmatic 
groups contributing to Gould’s high disparity levels. 

Delle Cave & Simonetta (1991) analyzed previous stud- 
ies in a well illustrated and comprehensive account of early 
Paleozoic arthropods. They emphasized the importance of 
functionality, specially the the role of feeding appendages in 
the evolution of arthropod morphotypes. For the most part, 
their taxonomic groupings and evolutionary charts bring 
perceptive and cohesive insight to some mini-groups (e.g., 
trilobitomorphs, the Sanctacaris problem, and the Scanian 
larval stages), and stress the need for authors to name new 
taxa, whatever the later higher categories might be. How- 
ever, they did not differentiate between food gathering and 
feeding (masticatory) roles and, as summarized in their 


AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 4 


Table IV, apparently missed the significance of relationships 

within the Dicephaiosomala and the overall relationships 

between anomalocarids and primitive trilobitomorph as- 
semblages (which they did recognize) such as the Yohoiida 
and Leanchoiliida. Briggs et al (1993) continued with a 
conservative classification of early arthropods (p. 6) in 
which several previous higher taxa were not recognized and 
the anomalocarids omitted entirely. Whatever the merits or 
weaknesses of these various treatments, collectively they 
underscore the state of flux that presently characterizes early 
arthropod classification. 

The purpose of this paper is to provide a classification 
that reflects more closely the actual degree of biological 
disparity and the major evolutionary themes within the 
Cambrian arthropod fauna. It also attempts to reveal, in more 
detail than previously, the relationship between form and 
food-gathering and feeding functions in selected Lower and 
Middle Cambrian arthropods and their descendent groups. 

ACKNOWLEDGEMENTS 

This study has taken place during a 10-year association 
with Dr Desmond E. Collins at the Royal Ontario Museum 
(ROM), Toronto, for whose tactful guidance and perceptive 
stimulus the writer is most grateful Dr David Rudkin 
(ROM), Derek Briggs (University of Bristol, U.K.), Jan 
Bergstrom (Natural History Museum, Sweden), Jarmila Kuk- 
alova-Peck (Carleton University, Ottawa), Frederick R. 
Schram (Institute of Taxonomic Studies, Netherlands) and 
several others, have directly or indirectly provided helpful 
input to the text. Earlier drafts of the text have been helpfully 
reviewed by C.R.Harington and Stephen Cumbaa (Canadian 
Musem of Nature (CMN), Ottawa), Murray Copeland and T. 
E. Bolton (Geological Survey of Canada (GSC), Ottawa), 
and A. L. Hamilton (Biosystematics, Agriculture Canada). 
Lisa Bohach (Earth & Ocean Sciences, University of Victoria) 
has provided perceptive commentary and editorial services, 
and references not previously available to the author. 

In the preparation of composite illustrations here I have 
been privileged to adapt, with warmest appreciation, the or- 
iginal text illustrations of D. E. G. Briggs, H. B. Whittington, 
D. E. Collins, F. R. Schram, X. Hou, L. Delle Cave, A. 
Simonetta, and several other primary sources. 

In parallel to the present study, Professor Edward Laidlaw 
Smith, San Francisco, CA, has combined and collated pre- 
vious arthropod categories in a detailed phyletic classific- 
ation of arthropods (Atlas of Insect Anatomy, unpublished). 
Since this study has resulted in some similar classificatory 
conclusions. Dr Smith has generously permitted detailed 
reference to and use of updated non-insect arrangements in 
this text, for which I am most grateful. 

SYSTEMATIC PREAMBLE 

The term “arthropod” is here defined as an invertebrate 
having an externally segmented body that bears one or more 
pairs of j ointed appendages. The body consists of head and 


trunk regions, of which the latter may be tagmatized or sub- 

divided into thorax and abdomen, mesosome and metasome, 

pygidium and/or telson, according to the taxonomic group. 
In primitive aquatic arthropods, the head always bears an 
acronal segment (first, or protocerebral somite) that is always 
pre-oral in position, having sensory organelles but no jointed 
limbs. The first true head segment (second or deutocerebral 
somite) is limb bearing, and usually pre-oral in active life 
stages. The head may also encompass up to five (rarely six) 
additional limb-bearing segments, the first of which (third or 
tritocerebral somite) may appear pre-oral in position. The 
post-oral appendages of head and trunk are primitively or 
embryologically biramous, the segments of which are exter- 
nally chitinized, sclerotized or mineralized. The inner ramus 
is usually locomotory, food gathering or masticatory, and the 
outer ramus usually respiratory in function. Growth pro- 
ceeds by moulting of the ectoderm (ecdysis). Following 
Bergstrom (1986, 1987) and Chen et al. (1994), true arthro- 
pods here embrace the primitive Cambrian dicephalosomatid 
genera Anomalocaris, Opabinia, Cassubia and close rela- 
tives. However, contrary to the views of Snodgrass (1956) 
and Manton (1977), true arthropods do not include the 
Tardigrada nor the Onycophora in which the body is not 
externally segmented and the post-oral limbs, although 
dactylate (clawed), are not jointed nor biramous. 

The Middle Cambrian macro-arthropod fauna is charac- 
terized by a high percentage of primitive body forms that, 
superficially, appear to be intermediate between true worms 
(phylum Annelida) and higher groups of aquatic arthropods 
such as the Chelicerata and Crustacea. Paradoxically per- 
haps, some of these early forms (e.g., Opabinia) show a 
remarkably high degree of specialization of body form and 
function that tends to mask their true phyletic affinities. In 
adult stages of some primitive modem arthropods (e.g., 
Remipedia) and larval stages of cirripedes, phosphatocopine 
ostracods and skaracarids, the acronal segment bears conspic- 
uous frontal organs or frontal filaments of presumed sens- 
ory function, and/or a median naupliar eye (Schram, 1986). 
The acronal somite is especially well developed in skaracarid 
crustacean larvae (e.g., Martinssonia Muller & Walossek, 
1986). However, in arachnids, myriapods and hexopods, the 
acron is considered embryonic and fused with the second 
head somite in active hfe stages (Savory, 1964). 

The first tme head segment (second somite) of arthro- 
pods bears one pair of limbs, of 1-14 basic segments, that is 
embryonically uniramous and pre-oral. These limbs may be 
stout, the segments spinose or toothed, or apically pincer- 
like and raptorial in function, as in chelicerates and their 
presumed precursors. However, more often they are 
filamentous and sensory in function, as in the "antennae" of 
trilobites, and the antennules of crustaceans and their pre- 
sumed ancestors, and marrellomorphs. In some Cambrian 
arthropods (Q.g., LeanchoiliaX the appendage appears distally 
multi-flagellate. In higher cmstaceans (Malacostraca), the 
antennules are often secondarily biramous (e.g., in 
Eumalacostraca), and occasionally triramous (in Stom- 
atopoda). In myriapods and insects, the antennae are 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 

uniramous, filamentous and sensory. In no instance, however, 
are these appendages gnathobasic. 

The third head somite (rarely lacking except in a few 
Cambrian species such as Opabinia and Sidneyia) bears a 
pair of limbs homologous with the antennae of crustaceans 
and early biantennate arthropods. These limbs, homologous 
also with the pedipalps of chelicerates and pycnogonids, 
may be uniramous or, as in the intercalary (supralingual) 
segment of myriapods and hexapods, vestigial or essentially 
lacking. In primitive arachnids and early precursors, and in 
larval stages of crustaceans, limbs of the third head somite 
are masticatory as well as locomotory and/or respiratory in 
function. Thus, as will be demonstrated in Cambrian 
aquatic arthropods (below), the evolutionary trend in func- 
tioning of the first two pairs of appendages in arthropods 
progresses from food gathering and mastication, to food 
sensing and tactilility. 

The head segment and limb homologies employed in 
this study, and suggested classification (pp. 23-27), conform 
with classical concepts of arthropod head structure, innerva- 
tion and embryology (e.g., of Borradaile & Potts, 1941; 
Savoiy, 1964; Bergstrom, 1979). Kukalova-Peck (1987) 
and Smith (1990) have fused the acronal segment of hexa- 
pods with the labrum to form the clypeolabral, or first 
(protocerebral) somite which, in Upper Carboniferous 
monurans, appears basolaterally segmented. The second 
head somite remains the antennal (deutocerebral) somite, 
homologous with the antennular somite of crustaceans. 
However, Smith (loc. cit.) has suggested that the chelicerae 
of arachnids originate on the third (tritocerebral, supralingual) 
somite, and the pedipalps on the fourth or mandibular seg- 
ment, resulting in eight prosomal somites, one more than the 
normal maximum recognized by all other authors. 

In Cambrian arthropods, the anterior portion of the gut 
is typically deflexed and the mouth usually opens ventrally 
on the head. In a few groups, however, (e.g., Jianfengia, 
Sanctacaris) the mouth appears to open apically or frontally 
(Hou, 1987a, Biiggs & Collins, 1988). Body segmentation 
may not always be externally visible, especially in larval 
forms, or in highly modified adults (e.g., some internal 
parasites). Paired limbs of the trunk are primarily biramous, 
but may be secondarily uniramous. The branches may be 
variously modified, unsegmented, or lacking (e.g., in early 
growth stages and in adults of various taxonomic groups). 
Thus, in a biramous limb, the outer branch may be lightly 
chitinized and flaplike (unsegmented) in swinuning forms 
or, when the outer is respiratory in function, the inner branch 
may be fully segmented, leglike, and heavily calcified or 
mineralized, especially in heavy bodied benthic forms. As 
noted above, some post-oral paired appendages may be 
gnathobasic wherein the coxa and/or adjacent segments are 
medially toothed, or the entire limb reduced and modified as 
a specialized mouthpart (e.g., mandible or maxilla). Such 
feeding appendages are tagmatized as part of the cephalon. 

Morphological differences between major groups of 
arthropods are fully as great as between accepted subphyla 


5 

and classes within other major phyla (e.g., as between 
chitons and cephalopods within phylum Mollusca). In 
Lower Cambrian to Lower Ordovician times (530-500 
m.y.b.p.), major groups of arthropods having modem repre- 
sentatives (e.g., Chelicerata, Crustacea) were then in what 
might be termed a primordial or early state of evolution or, 
in the case of Myriapoda and Hexapoda, unrecognized as 
such. Thus, true crustaceans were represented in the Cambrian 
fossil record only by the Maxillopoda (Ostracoda, Cirripedia, 
and skaracarid larval forms) (see Schram, 1986 in part; Dahl 
1984, 1987). Members of the Aglaspida (Upper Cambrian) 
were considered by Bergstrom (1979) to be early chelicerates 
but Briggs et al. (1978) demonstrated the filamentous nature 
of the "chelicerae" and removed the Aglaspidida from the 
merostomes. The earliest chelicerates are Chasmataspis, or 
perhaps Triopus, from the Lower Ordovician (Fig. 8). Other 
major arthropod groups (e.g. Myriapoda, Hexapoda) were 
recognizable in late Silurian and early Devonian times, when 
freshwater and terrestrial fossils deposits were first identiifed. 

PREVIOUS CLASSIFICATIONS 

Several different classifications of Cambrian macro- 
arthropods have been proposed, four of which are presented 
in Table 1. The 17 sample species listed here were classified 
initially by Walcott (1912) who “shoehorned” them (fide 
Gould, 1989) into a relatively few existing crustacean and 
arachnid subcategories (Column 1). Over the next 75 years 
the species were classified variously by Stdrmer (1959), 
Sharov (1966) and Bergstrom (1979), and incorporated by 
Edward Laidlaw Smith in a forthcoming “Atlas of the 
Insecta”, communicated to the writer, with kind permission, 
for comparative purposes here (Column 4). Despite previous 
designations, Gould (1989) regarded these forms as highly 
distinctive, belonging to two new phyla; 12 unique arthropods; 
one chelicerate arthropod; one trilobite; and one malacost- 
racan (Column 2). Briggs et al.( 1993) had retreated into a 
somewhat similar conservative listing of Cambrian 

arthropods, a list that did not include Opabinia, 

and other dicephalosomatid forms (Column 3). The E. L. 
Smith listing (Column 4) would place 15 of Gould's new or 
unique taxa within long-established classes of crustaceans, 
trilobitoids, protochelicerates, and chelicerates, five of them 
more or less within Walcott's original categories. However, 
as we may note in the following text, Smith's placement of 
Marrella mdBranchiocaris within the protochelicerates, 
and Odaraia andCanadaspis within the Crustacea, is inter- 
preted otherwise here. 

Mechanisms of food-pgathering and feeding. 

In assessing the overall legitimacy of these classifications, 
we might conclude that, under the circumstances of the 
relatively limited systematic knowledge of his day, Charles 
Walcott was remarkably perceptive in much of his classifi- 
cation. Although thereticenceofGouldandBriggstorefine 


AMPHIPACMCA VOL. 11. NO. 1 AUG. 31, 1995 6 


TABLE L THE CLASSIFICATORY STATUS OF SOME BURGESS SHALE FOSSIL GENERA 


Genus Name 

Higher category by Author 


Walcott (1912) 

Gould (1989) 

Briggs et al (1993) 

E.L.Siiiith C'Atlas" prep)* 

Marrella (Wale.) 

near Trilobita 

unique 

Arthropod 

Protochelicerata Stormer, 1944 



arthropod 

(primitive) 

CL. Marrellidea Walcott 1912 

Yohoia (Wale.) 

branchiopod 

unique 

Arthropod 

Protochelicerata Stprmer, 1944 


crustacean 

arthropod 

(other) 

CL. Yohoiidea Henriksen 1928 

Opabinia (Wale.) 

branchiopod 

new 

Unassigned 

Protochelicerata Stprmer, 1944 


crustacean 

phylum 

Invertebrate 

CL. Probosciferidea Sharov 1966 

Burgessia (Wale.) 

branchiopod 

unique 

Arthropod 

Trilobitoidea St0rmer, 1955 


crustacean 

arthropod 

(other) 

0. Nectaspida Raymond, 1920 

Branchiocaris (Wale.) 

malacostracan 

unique 

Arthropod 

Protochelicerata St0rmer 1944 


crustacean 

arthropod 

(primitive) 

CL. Branchicaridea 

Canadaspis (Wale.) 

phyllocaridan 

malac- 

Crustacea 

Crustacea Pennant 1777 


crustacean 

ostracan 


CL. Branchiopoda Latr. 1817 

Naraoia (Wale.) 

branchiopod 

soft-bodied 

Trilobita 

Trilobitoidea St0rmer, 1955 


crustacean 

trilobite 


0. Nectaspida Raymond 1920 

Odaraia (Wale.) 

malacostracan 

unique 

Crustacea 

Crustacea Pennant 1777 



arthropod 


CL Pranchiopoda Latreille, 1817 

Sidneyia (Wale.) 

merostome 

unique 

Arthropod 

Protochelicerata St0rmer 1944 



arthropod 

(other) 

CL. Sidneyiidea Walcott, 1912 

Malaria (Wale.) 

merostome 

unique 

Arthropod 

Trilobitoidea St0rmer, 1955 



arthropod 

(other) 

incertae sedis 

Habelia (Wale.) 

merostome 

unique 

Arthropod 

Trilobitoidea Stprmer, 1955 



arthropod 

(other) 

incertae sedis 

Actaeus (Wale.) 

unknown 

unique 

Arthropod 

Protochelicerata St0rmer, 1944 



arthropod 

(other) 

CL. Leancholiidea Raymond! 

Alalcomanaeus (W.) 

unknown 

unique 

Arthropod 

Protochelicerata St0rmer, 1944 



arthropod 

(other) 

CL. Leanchoiliidea Raymond! 

Emeraldella (Wale.) 

merostome 

unique 

Arthropod 

Protochelicerata St0rmer, 1944 



arthropod 

(other) 

CL. Emeraldellidea Raymond! 

Leanchoilia (Wale.) 

branchiopod 

unique 

Arthropod 

Protochelicerata St0rmer, 1944 


crustacean 

arthropod 

(other) 

CL. Leanchoiliidea Raymond! 

Sanctacaris (Briggs & 

N/A 

chelicerate 

Chelicerata 

Chelicerata Heymons 1901 

Collins) 



arthropod 

Arachnida Lamarck, 1801 

Anomalocaris (Wale.) 

branchiopod 

new 

Unassigned 

Protochelicerata St0rmer, 1944 

-1- Laggania 


phylum 

Invertebrate 

CL. Anomalocaridea Raymond! 

+ Peytoia 





+ appendage F ^ 

Selected names with permission of E. L. Smith (references not detailed here); ! - Raymond, 1935. 


the classification with new terminology is to some extent 
justified, Smith's listing of previous formal categories indi- 
cates that their reticence does not provide a helpful solution 
to the problem. The need seems greatest for more careful 
and more rigorous definition of existing categories, based on 
principles of functional morphology where possible, and a 
resort to new categories when existing or redefined catego- 
ries prove inadequate. As Gould (per Schram, 1990) reminds 
us, errors and oversights of the past are part of the process 
of getting the probably correct answer, and so provide a 
prime stimulus for the present undertaking. 

Gould (1989) noted that previous workers on Cambrian 
arthropods seemed reasonably confident of their classifica- 
tion of the most primitive forms, e.g., the Onycophora, and 
the presumably most advanced major taxon, the Trilobita. 


However, they seemed less certain of other arthropods 
variously attributed to the Crustacea (ie. Canadaspidida, 
Branchiocarida) or having only general similarities with the 
Trilobita. The greatest difficulties were encountered with 
forms having both annelid-like and arthropod-like features 
(e.g. Anomalocaris, Opabinia). Charles Walcott (1912) 
utilized subcategories of extant arthropod groups (e.g., 
Branchiopoda, Ostracoda -t- Merostomata). St0rmer(1944, 
1959) proposed new “catch-all” categories (e.g., Trilobit- 
oidea) for many enigmatic forms. These classifications 
utilized standard character states such as body tagmatization, 
number of paired head (or head shield) appendages, types of 
appendages (biramous, gnathobasic, gill-like) and larval 
biology, to the hmit of existing knowledge, but did not 
emphasize fimctionahty or possible behavioural significance. 


AMPHIPACIFICA VOL. U. NO. 1 AUG. 31, 1995 


7 


Bergstrom (1979, et seq.) employed the term 
“Schizoramia” to encompass all Trilobitomorpha (Trilobita, 
Merostomatoidea, and Chelicerata). These are characterized 
by primitively biramous trunk limbs of which the endopod is 
gnathobasic, and the exopod bears lamellar spines. The 
enigmatic genus Emeraldella, having gnathobasic post-oral 
legs, was included here, as well as the Marrellomorpha, but 
the latter group primarily lacks gnathobasic limbs. The 
Pycnogonida (Pantopoda) was not related to any particular 
arthropod group. Commendably, Bergstrom relegated 
binia and Anomalocaris to the status of a “pre-arthropod” 
stock, but later (1986, 1987) decided they were indeed 
arthropods, a view now firmly supported by the recent work 
of Chen eLal (1994). However, Bergstrom employed the 
term Uniramia to encompass both the soft-bodied, externally 
annulated onychophorans, and the hard-bodied, externally 
segmented myriapods and hexapods having whole-limb 
jaws. This concept is now proving flawed and untenable as 
a category of natural classification (see Kukalova-Peck, 
1992). Onychophorans, early forms of which did exist in 
Cambrian seas, resemble the Tardigrada in having shaft-like, 
primitively uniramous limbs and pharyngeal teeth or spines, 
whereas myriapods and insects have segmented, primitively 
biramous limbs, and mouthparts modified from biramous 
limbs. Furthermore, Bergstrom’s doubts that biramous and 
mandibulate crustaceans arose from the same gnathobasic 
limb stock as hexapods are not supported here nor by some 
other workers (e.g., Kukalova-Peck, 1987). Imperfect 
fossilization has so far prevented determination of the precise 
nature of locomotory limbs of dicephalosomatids However, 
such is not here considered a major impediment to phyletic 
implications of the better preserved, clearly "arthropodized" 
feeding appendages of the head region, nor overall relation- 
ships with confirmed early biramous arthropod groups. 

In assessing the impact of feeding processes on the 
evolution of body form in arthropods, a definition of terms 
is prerequisite. The entire feeding process encompasses 
food-gathering and food-consumption mechanisms. The 
food-gathering mechanism is the process by which food 
items are entrapped and brought to the mouth region. The 
food-consumption (feeding) mechanism is the process of 
mastication, the external means by which food items are 
rendered suitable for entry into the digestive tract proper. 

Basic types of feeding processes of arthropods and their 
presumed antecedents are illustrated in Fig. 1. In errant 
poly chaete worms (Q.g.^Nereis, Vefit/iej), a taxonomic group 
"classically” presumed ancestral to the arthropods, the head 
consists of a prostomium and usually a peristomial segment 
bearing food-sensing tentacles. No paired limbs, segmented 
or otherwise, are involved in food gathering or in food 
mastication; these processes are entirely pharyngeal (Fig. 
lA). The mechanism consists of an eversible pharyngeal 
proboscis, the everted distal end of which is armed with 
strong teeth or “jaws” by means of which the food material 
(prey organism) is captured and killed. As the proboscis 


retracts, it re-inverts, taking in the prey and partly macerating 
it by means of other teeth lining the pharynx wall. The food 
is then passed rearward to the digestive gut proper. No true 
arthropods conform with this category. 

In very primitive uniantennate arthropods, (e.g., 
Anomalocaris, Fig. IB . 1 ), food is gathered by the large, spin- 
ose and multi-segmented, pre-oral paired appendages. These 
capture and transfer prey organisms posteriorly to the mouth 
region that opens immediately behind the first true head 
segment. The actual feeding mechanism, however, remains 
entirely pharyngeal; no paired mouthparts or leg gnathobases 
are present, although in the related Opabinia regalis (Fig. 
1B.2), some prey items may be partly macerated by the pre- 
oral clawed appendage. In the anomalocarids, food is initi- 
ally macerated by means of peribuccal teeth, and/or stout 
teeth or spines lining the anterior walls of the pharynx, as in 
some polychaetes. This feeding process is analogous, or 
perhaps even homologus, to mechanisms elsewhere among 
living arthropods in the pycnogonids, and among other 
invertebrates in the cephalopod molluscs (Borradaile & 
Potts, 1941). In cephalopods, the “head-foot” appendages 
(tentacles) grip, but do not masticate, the prey by means of 
specialized suckers, rather than spines; modified anterior 
pharyngeal teeth, the horny beaks, and smaller radular teeth 
masticate the prey items just inside the mouth entrance. 

In more advanced uniantennates (e.g. in chelicerates. 
Fig. 1C), food gathering is also the prime function of post- 
oral head (prosomal) appendages, and/or the cheliform pair 
of pre-oral appendages. In primitive aquatic chelicerates 
(e.g., merostomes), the food is first macerated externally by 
means of a grinding action of the gnathobasic coxae of the 
paired head and/or trunk appendages. In more advanced 
terrestrial arachnids that secondarily lack leg gnathobases, 
the killing bite and maceration of the prey is performed by the 
distally clawed first post-oral appendages, the pedipalps and/ 
or the pre-oral chelicerae (Savory, 1964). 

Within advanced biantennate (mandibulate) arthropods 
(e.g., malacostracan crustaceans. Fig. ID), the pre-oral and 
first post-oral appendages are flagellar and food-sensing. 
Food is gathered mainly by the anterior trunk (thoracic) 
limbs. Swimming, and often respiratory functions may be 
relegated to the posterior trunk (abdominal) limbs. Food is 
macerated by specialized post-oral limbs of the head region, 
the mandibulate mouthparts. Other branches or lobes of 
post-oral head appendages may serve in locomotion, and/or 
respiration, especially in adults of more primitive groups 
(e.g., cephalocaridans) and in larval stages of advanced 
forms. Food mastication may also become the primary func- 
tion of one to three pairs of anterior trunk limbs, serving as 
maxillipeds (e.g., in Decapoda), or as gnathopods (e.g., in 
Amphipoda). In their larval stages (e.g., nauplii, metanauplii) 
the biramous first post-oral appendage (antenna 2) usually 
retains a function in food gathering and mastication, as well 
as locomotion (Schram, 1986). 


AMPHIPACMCA VOL. D. NO. 1 


AUG. 31, 1995 8 


oc;ipitot onttnnoi 



RAPTORIAL TEETH 
(JAWS) 

PARAGNATHS 
(LATERAL TEETH) 


A. PHARYNGEAL 


PRE-ORAL HEAD LIMB 
(CHELICERA) 


RAPTORIAL 
PRE-ORAL LIMB 


RAPTORIAL "CLAW" 
(FUSED PRE-ORAL 
HEAD LIMBSl 




-ORAL 
HEAD LIMBS 
(MOUTH - 
PARTS) 


POST-ORAL 
HEAD LIMBS 
(GNATHOBASIC) 


Limulus 

C. CHELICERATE PRE-ORAL 
GNATHOBASIC POST-ORAL 


TRUNK LIMBS 
( GILL BOOKS ) 


GILL BOOKS ANUS ANUS 


PLEOPODS 


ANUS 


TELSON ■ 


Orconectes 


D. ANTENNAL PRE-ORAL 
MANCHBULATE POST-ORAL 


FIG. 1. BASIC TYPES OF FOOD-GATHERING AND FEEDING MECHANISMS IN AQUATIC 
ARTHRO PODS. A. Polychaete (ancestral). B. Primitive uniantennate arthropod. 
C. Advanced uniantennate arthropod D. Advanced biantennate arthropod 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 9 


TABLE II. SELECTED GENERA OF CAMB RIAN UNIANTENNATE ARTHROPODS 
CATEGORIZED BY FOOD- GATHERING AND FEEDING MECHANISMS 


SEGMENTED LIMBS 
LACKING 

1 . 

SEGM 

ENTED PRE-AND POST-ORAL LIMBS 

II. 

PRE-ORAL LIMBS 
RAPTORIAL 

Ml 

PRE-ORAL LIMBS 
TRANSITIONAL 

IV. 

PRE-ORAL LIMBS 
FILAMENTOUS 

V. 

PRE-ORAL LIMBS 
CHELICERATE 

PHARYNGEAL 

MASTICATION 

PHARYNGEAL 

MASTICATION 

TRANSITIONAL 

PHARYNGEAL 

MASTICATION 

GNATHOBASIC 

MASTICATION 

GNATHOBASIC 

MASTICATION 

POLYCHAETA 

TARDIGRADA 

ONYCHOPHORA 

Halluctgonia 

AyshaaSa 

ENDOPODS LOBATE 

OR SMOOTH 

Anomalocaris 

Laggania 

Opabinia 

t Tulllmonstrum 

Casaubla 

Jianfengia 

Yohoia 

ENDOPODS SPINOSE 

Leanohollla 

Acanthomaridlon 

Actaeus 

Alalcomanaeua 

Sldneyla 

Burgessia 

Molaria 

Habelia 

Tegopelte 

Naraola 

TRILOBITA 

Sanctacaris 

Emeraldella 

Aglaapis 

Chaamataapla 
t MEROSTOMATA 
t EURYPTERIDA 
t 8CORPIONIDA 

t PYCNOGONIDA? 


t Ordovician and later 

Selected uniantennate arthropods of the early Paleozoic 

are grouped according to categories of food gathering and 
feeding outlined in Table II. As noted previously, unassisted 
pharyngeal feeding typifies polychaetes and pararthropods 
such as the tardigrades and onychophorans (Column I). The 
dicephalosomatid arthropods (Column II) utilize only rap- 
torial pre-oral appendages in food gathering and/or prelimi- 
nary food mastication. They feed in an essentially similar 
pharyngeal manner, except that the mouth opening is deflexed 
ventrally in anomalocarids and proboscoideans, and opens 
anteriorly (or nearly so) in Yohoiida (Hou, 1987a). In prim- 
itive trilobitomorphs, the Leanchoiliidacea (Column III), the 
post-oral head and trunk limbs appear capable of capturing 
and holding food items but feeding is still essentially pharyn- 
geal. In the advanced species Alalcomenaeus, post-oral 
limbs are essentially gnathobasic (Delle Cave & Simonetta, 
1991). In advanced trilobitoideans, includin Sidneyia, the 
Burgessiida, trilobites, Emeraldellida and Sanctacarida (Col- 
umn IV), the pre-oral appendages become essentially singly 
filamentous in form and presumably chemosensory and 
thigmotactic in function. The post-oral head and trunk limbs 
become fully gnathobasic (although remaining biramous) 
and presumably assisted in both food capture and food 
mastication. The chelicerates are a final stage in the uni- 
antennate feeding series (Column V). The raptorial pre-oral 
limbs are reduced to two to four segmented chelicerae, and 
the post-oral head limbs are fully gnathobasic and essentially 
uniramous. Both types of head appendages may assist in 
food gathering and food maceration, especially in the terres- 
trial arachnid subgroups. The anterior post-oral trunk limbs 
are essentially uniramous; the endopod is lost, but the exopod 
remains functional in respiration. 

This tabular arrangement of taxa according to feeding 
style parallels an increasing evolutionary sophistication of 
head and trunk segmentation, and form and function of their 
appendages as detailed in pages 11-14. It also matches the 


? Head limbs not gnathobasic 

fossil track record of the uniantennate groups (Table V, p. 
28). Thus, the most primitive feeding styles, as in the 
dicephalosomatids, persisted little beyond the Cambrian 
Period and not beyond the Palaeozoic Era. By contrast, the 
most advanced uniantennate feeding types expanded into the 
chelicerate taxa of Ordovician and later periods, including 
the remarkably diverse terrestrial arachnids of Tertiary and 
Recent times. 

Evolution of Post-oral Limb Morphology 

The changing structure of the post-oral head and trunk 
appendages of uniantennate arthropods is depicted in greater 
detail in Figure 2. Within the Dicephalosomatida, the 
Anomalocarida and Probosciferida were equipped with pairs 
of closely approximated paddlelike plates on each side, not 
clearly joined at the base, and perhaps not technically, even 
if functionally, forming a biramous limb. The upper plate 
(in Opabinm, Fig. 2B, C) was fringed with lateral lamellae, 
presumably respiratory in function. The head of Opabinia 
(2B, C; 7C.l)lacked post-oral plates, but the three pairs of 
post-oral head plates in Anomalocaris (Fig. 2 A) are consid- 
ered homologus with the trunk plates. In Cassubia (Fig. 3), 
considered here (and by Smith, "Atlas" unpubl.) as a benthic 
anomalocarid with relatively short stout pre-oral limbs, the 
head may be two segmented. Trace elements alongside the 
trunk may be ambulatory endopods of the posterior head and/ 
or anterior trunk segments. In Yohoiida, including the multi- 
segmented Jianfengia from the Lower Cambrian of China 
(Fig. 7G), the head bore 3 pairs of post-oral appendages of 
which the endopod was 7-segmented, cylindrical, and pre- 
sumably ambulatory. The limbs were not demonstrably 
gnathobasic, but the ectoderm was sclerotized or mineralized, 
with a gill-like exopod, much as in a trunk limb of the 
biantennate genus Marrella (Fig. 2D). An exopod was 
present andfoliaceous in head limbs of the ^longnt^ Jianfengia 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 10 






FIG. 2. BILOBATE AND BIRAMOUS POST-ORAL (HEAD AND TRUNK) LIMBS 
OF PRIMITIVE ARTHROPODS OF THE EARLY PALEOZOIC ERA. 

A. Anomalocaris (section) B. Opabinia (dorsal) C. Opabinia (lateral) 

D. Marre(&i(trunk section) E. ( post-oral section) F. L. (trunk section) 

G. Sidneyia (post -oral section) H. TnorlArus (trunk limb) J. LimulusQeRl) 


AMPHIPACIFICA VOL. D. NO. 1 AUG. 31, 1995 


11 


but apparently lacking in those of the relatively short-bodied 
and more advanced Yohoia. Trunk limb exopods were 
broad, as in the trilobitomorph Leanchoilia (Fig. 2E, F), and 
margins setose, as in Sanctacaris (Fig. 6). At least the first 
pair, and possibly up to 1 0 pairs, of anterior trunk limbs bore 
a cylindrical ambulatory endopod. 

Within the primitive transitional trilobitomorphs, in- 
cluding the Leanchoiliidacea and Actaeida (Figs. 2E, F), the 
3 pairs of post-oral head limbs, and all trunk limbs, developed 
strong spines on the inner margins of the segments of the 
endopod. The spines were presumably used in grasping and 
holding prey organisms, much in the manner of the thoracic 
leg spines of eusirid amphipods and adult dragonflies. In 
more advanced groups of trilobitoids, the post-oral hmbs of 
head and trunk became fully gnathobasic, in which strong 
teeth or spinose processes developed on the proximal (coxal 
and basal segments) of the endopod. The distal claws of the 
endopods functioned in seizing, and the gnathobases in 
killing and masticating, prey items prior to transfer to the 
mouth proper. In Sidneyia (Fig. 5D), the head lacked post- 
oral limbs but the anterior four pair of trunk limbs were 
strongly gnathobasic and uniramous, the remaining trunk 
limbs biramous. In Burgessiida and in the Trilobita proper 
(Fig. 2H), the 3 pairs of post-oral head limbs remained fully 
biramous and multifunctional. The outer ramus bore numer- 
ous respiratory lamellar spines. In the Emeraldellida, includ- 
ing Emeraldella (Figs. 6E, 7M) and Sanctacaris (Figs. 6, 7L) 
the anterior two trunk segments became fused to the head, 
resulting in 5 pairs of post-oral head appendages. As the 
locomotory and respiratory functions decreased and rapto- 
rial and masticatory functions of the head limbs increased, 
the endopods became more powerfully raptorial and 
gnathobasic, whereas the exopods became vestigial, as in 
Sanctacaris. In the aquatic chelicerates, the merostomes 
(e.g. Limulus, Fig. 2J), the head region similarly bear five 
pairs of strongly gnathobasic, ambulatory and essentially 
uniramous limbs. However, the pre-oral limbs of merostomes 
are chelicerate, not filamentous, and derived from very 
different ancestral uniantennates (seepage 12). In all but the 
most prinutive aquatic merostomes, the trunk endopods lost 
their ambulatory function and disappeared, whereas the 
anterior pairs of trunk exopods remained functional in the 
form of book gills and, in terrestrial derivatives, book lungs. 

In the above evolutionary sequences, the development 
of gnathobasic limbs may have been a consequence of im- 
proved efficiency in exploiting, as food, hard-shelled prey 
living in soft bottom sediments. The feeding style of 
Limulus still follows this original primitive pattern. 

Evolution of Food-Gathering Appendages 

Within uniantennate arthropods, the morphological and 
functional forms of pre-oral food-gathering and food-sens- 
ing appendages may be linked in possible evolutionary path- 
ways (Fig. 3). The presumed ancestral form of this 
cephalopod-style food-gathering mechanism is the large 
multi-segmented raptoral form typical of species of Anomalo- 


caris (Figs. 3A, D). Despite anomalies of fossil limb pre- 
servation, the primary plane of motion is presumed to be 
essentially vertical. The paired limbs combined, nearly in 
parallel, to form a raptorial basket in which prey organs were 
captured and killed by the daggerlike posterior (inner) mar- 
ginal spines (Collins, 1987). The food items were then 
transferred posteriorly, by deflexion and retraction of limbs, 
to the masticatory buccopharyngeal teeth of the mouth 
region. This plane of action contrasts with the nearly 
horizontal or oblique position of the natatory trunk limbs or 
lateral lobes of epi-benthic animals. In benthic species, in 
which the endopods of post-oral head and trunk limbs were 
mainly ambulatory and vertical in position, the pre-oral 
appendages were essentially co-planal. In "Laggania "-like 
animals (Table I - A. nathorsti group), with 11 -segmented 
limbs, the posterior marginal spines were exceptionally long 
and strong, as if utilized in raking or digging in soft sediments 
(Fig. 3D). 

If the plane of action is rotated to the horizontal, the 
paired limb spines come into opposition as a prey-capturing 
and killing mechanism. In this manner, and through prolon- 
gation of the head region into a long flexible annulated pro- 
boscis, the terminal raptorial claw of ^the free-swimming 
Opabinia can be derived (Fig. 3B; Bousfield & Collins, in 
preparation). The paired spines on each side are 14 in 
number, as in Anomalocaris canadensis. The distal five of 
these are longer and more steeply oblique and probably 
served in prey capture, whereas the proximal nine pairs are 
stouter, shorter, and more perpendicular and may have 
served in holding, crushing, and possibly preliminary mas- 
tication. The form and function of the claw is analogous to 
a modern pair of pliers. However, it was probably activated 
by a combination of muscular and hydrodynamic processes. 
The transfer of food material rearwards to the mouth by the 
proboscis was probably similar to the action of an elephant’s 
flexible trunk. The proboscis does not contain the anterior 
gut, as proposed by Sharov (1966) (per Callahan, 1979). 

In a much more highly modified Upper Carboniferous, 
internally segmented, squidlike counterpart, Tullimonstrum 
gregarium, described in detail by Johnson & Richardson, 
1969 (Fig. 7C.2), the terminal claw was more slender, and 
the spines, 13- 14 in number on each side, were minute (Fig. 
3C). Prey items were probably small and soft-bodied, 
possibly free-swimming plankters, or worms or insect larvae 
extracted from tubes in soft bottom sediments. 

In a Lower Cambrian benthic species, Cassubia infra- 
cambriensis (Lendzion, 1975), the number of pre-oral limb 
segments was reduced to 7, and segments 2-5 had large 
medial spinose processes (Fig. 3E). Regrettably, the plane 
of motion is not precisely determinable from the single in- 
complete fossil specimen. 

In a direction presumably leading to the chelicerates, 
the pre-oral appendage of the protochelicerates Jianfengia 
and Yohoia was reduced to 3-4 segments, the outermost 
being double-spined and movably pincering upon the inner 

marginal spine of segment 2 (Fig. 3F). Limb orientation was 

in a vertical plane and the movable distal spine had been 


AMPHIPACIFICA VOL. 11. NO. 1 AUG. 31, 1995 12 





FIG. 3. PLAUSIBLE EVOLUTIONARY SCENARIOS IN THE PRE-ORAL APPENDAGE 
OF UNIANTENNATE ARTHROPODS (from Gould (1989) and various sources) 

A. D. Anomalocaris spp. ( Hypothetical Ancestrai type) 

Raptorial proboscoid line B. Opabima C. Tullimomtrum (Carboniferous) 

Raptorial chelicerate line £. Cassubia F. Yohoia tenuis Gl. Limulus (late Palaeo 2 oic) 
Sensory flagellar line H. LeanchoiUa J. Actaeus K. Emeraldella 


rotated to the lower or inner side, as in limuloids and phal- 
angiate arachnids (Fig. 3G1). In eurypterids, scorpions, and 
pedipalpate arachnids (including spiders), however, the move- 
able segment is on the upper or outer side of the limb (Fig. 
3G2). A major link in the presumed lineage from Yohoia to 
merostomatid arachnids is not confirmed from the fossil 


record, viz., a yohoiid-like pre-oral appendage on a broad- 
ened head of 5 post-oral segments. 

A further evolutionary thrust of the pre-oral uniantennate 
limb resulted in a filamentous sensory flagellum, repre- 
sented in early stages by the form of the 7-segmented "great 
appendage" of LeanchoiUa (Fig. 3H). The inner marginal 



AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 13 



FIG. 4. PROPOSED HOMOLOGIES BETWEEN PRE-ORAL APPENDAGES OF MIDDLE CAMBRIAN 
TRILOBrrOMORPH UNIANTENN AXES AND ANTENNULES OF CRUSTACEAN fCIRRIPEDE AND 
ASCOTHORACID) BIANTENNATE ARTHROPODS (A,B,C after Gould, 1989 ; D, E, F after Schram, 1986) 


spines of segments 3-4 and the terminal spine of segment 7 

were apparently modified as a multi-segmented whip-like 
flagellum, whereas those of segments 5 and 6 were reduced 
to short stubs. In Actaeus (Fig. 7E.3), segments 3 and 4 
remained flagellated, but 5-7 were much shortened, and bore 
short spine-like processes. In Sanctacaris, segment 3 (?) was 
short-flagellate and (4?) 5-7 terminated in a star-hke cluster 
of spines (Fig. 4C; 6D). Derivation of a 3-segmented 
chelicera from such an appendage would seem improbable. 
The simple elongate flagellar state is attained in Alalcomeneus 
(Fig. 7E.4), Emeraldella (Fig. 3K) and in most other 
trilobitoids, including the Burgessiida and the Trilobita 
(Fig. 5E, F). 

This analysis concludes that, in some evolutionary lines 
within uniantennate arthropods, the pre-oral appendage was 
initially a raptorial food gathering apparatus that secondarily 
became flagelliform. These morphotypes, including the 
trilobites, did not persist beyond the Paleozoic Era. In the 
evolution of primitive merostomes (e.g. Chasmataspis), a 
filiform antenna is unlikely to have disappeared, and a 
cheliform appendage suddenly appeared, as Bergstrom (1979) 
proposed for early chelicerates. The pre-oral appendage was 
already semi-cheliform in the proposed ancestral Yohoia. 
The trend from raptorial to sensory flagellar condition within 
the Trilobitoidea, rather than the reverse, is accompanied by 


parallel evolutionary trends in cephahzation of the head, 
gnathobasic development of ambulatory limbs, rearward 
shift of respiratory limbs, and in other major character states 
within component major sub-taxa (p. 22). 

Within biantennate arthropods, however, the evolution- 
ary picture is different. As revealed by the limited early fossil 
record, and the ontogeny of larval stages of extant and fossil 
forms, the pre-oral appendage appears to been filiform 
thoughout, with few exceptions, as noted on page 14). The 
flagellate form has also persisted, with little change, in the 
myriapod and hexapod taxa that have dominated terrestrial 
environments since the close of the Paleozoic Era (Delle 
Cave & Simonetta, 1991). 

Possible Homologies in Pre-oral Appendages of 
Uniantennate and Biantennate Arthropods. 

As noted above, the significance of the first pre-oral 
appendage as a mechanism of food detection, food gathering, 
and general feeding style is basic in the Arthropoda. Both 
the organelles of the acron (e. g., frontal filaments, naupliar 
eyes) and the pre-oral first segmented head appendage are 
presumed sensors of environmental conditions and food 
sources. In uniantennates, the primary role ofthe latter was 
food gathering, a raptorial function that was retained in the 


AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 14 


single successful line of uniantennate evolution, the 
Chelicerata. In the biantennates, however, the appendage 
was primarily sensory, at an early stage, and remained so 
throughout evolutionary history of all major subgroups. A 
comparison of pre-oral limbs of selected primitive morpho- 
types of both uni- and bi-antennates is pertinent (Fig. 4). 

In the primitive trilobitomorphs, the pre-oral appendage 
passes through several stages of reduction of accessory 
flagella and sensory organelles (Figs. 4A, B, C). leading to 
the simple elongate flagellar condition of the Trilobita and 
Emeraldellida. In a few primitive maxillopodan crustaceans 
with specialized life styles, however, the appendages devel- 
oped correspondingly specialized sensory and raptorial func- 
tions. In cirripedes, the antennules are natatory in naupliar 
and metanaupliar larvae (Fig. 4D), but become organs of site 
selection and attachment in the cyprid larvae of sessile, shell- 
burrowing and parasitic forms, the Thoracica, Acrothoracica, 
and Rhizocephalia respectively (Glenner&Hoeg, 1995)(Fig. 
4E). These 4-segmented antennules bear aperhaps superficial 
but remarkable similarity, and almost certainly homologous 
relationship to, the pre-oral appendage of the primitive 
trilobitoiduniantennates, (Fig. 4B), andSanctacaris 

(Fig. 4C). 

However, in the ascothoracidan biantennates, parasitic 
on echinoderm and anthozoan coelenterates, the antennule 
is raptorial in the cyprid and adult stages (Fig. 4F). The term- 
inal two segments of the 4-segmented appendage, reminis- 
cent of Yohoia (Fig. 3F), form a subchela for attachment to 
the host, or removal of pieces of the host tissue as food. 

Perhaps a more precise concept of the pre-oral append- 
ages of long extinct uniantennates of the Cambrian Period 
might be derived through closer study of the antennules of 
these very primitive extant crustacean biantennates. 

The Pre-oral Appendage of Trilobitoid Uniantennates, 

The general external morphology of selected tiilob- 
itomorph uniantennates is shown in Fig. 5. In Burgessia 
(Fig. 5 A), Molaria (Fig. 5B) andHabelia (Fig. 5C), the head 
comprises four segments (five somites) which, in Burgessia, 
subtends a broad carapace covering the trunk segments. The 
post-oral appendages are ambulatory, those of the trunk also 
respiratory. The trunk terminates in a spikelike telson, 
similar to that of the merostomatid chelicerates, and suggests 
a strongly benthic life style. In Sidneyia (Fig. 5D), the head 
is only 2-segmented, but the anterior four trunk segments 
bear uniramous, powerfully gnathobasic limbs that are effec- 
tively part of the cephalic masticatory complex. The 
posterior 3 trunk segments are free and bear a broad, flabellate 
telson, evidence that Sidneyia was a powerfully swimming 
benthic and epibenthic predator. 

In the trilobites, [e.g., Naraoia , a "soft trilobite" (Fig. 


5E), and Olenoides, a primitive true trilobite (Fig. 5F)], the 
head is also 4- segmented, with 3 pairs of post-oral ambula- 
tory, respiratory, and masticatory head limbs, and 11+ pairs 
of similar trunk limbs. However, trilobites differ from Bur- 
gessiida in having a broad depressed head shield and trunk, 
the latter ending in a short pygidium or tail region of a 
variable number of segments. Both groups represent middle 
stages in cephalization of anterior trunk limbs. 

Sanctacaris 

On the basis of five well-preserved specimens from the 
Stephen Formation, near to but slightly younger than the 
Burgess Shale quarry, Briggs and Collins (1988) described 
a large carnivorous arthropod, Sanctacaris uncata, that they 
assigned to subphylum Chelicerata (Fig. 6). The broad head 
bears large eyes and six pairs of biramous appendages, the 
first five of which form a raptorial array of segmented, 
spinose and gnathobasic endopods with simple short 
antennalike exopods. The outer ramus of the sixth limb is 
also filamentous, but the inner ramus is short, terminating in 
a firinge of starlike radiating spines. The mouth is located 
anteriorly, presumably in a narrow gap between the first limb 
bases. The broad trunk is 11 -segmented, the posterior 
bearing a paddle-shaped telson, the anterior 10 each bearing 
paired biramous lim bs of which the exopod is large, flabellate, 
and natatory-respiratory in function. The inner ramus is 
slender, multi-segmented, and presumably ambulatory; 
marginal spines and/or gnathobases were not demonstrable. 

However, another interpretation is utilized here. The 
biramous "sixth" appendage (Fig. 6D), bears a striking 
resemblance to the "transitional" pre-oral limb of Actaeus, 
with its star-shaped accessory flagellum (Fig. 5B), but unlike 
the raptorial condition in Yohoiida (Fig. 3F; 7D) or the 
chelicerate condition in arachnids (Fig. 6F). Furthermore it 
arises near the eye, in a typically pre-oral position. The five 
pairs of raptorial head limbs of Sanctacaris have apparently 
been displaced forward beneath the head to form a raptorial 
"basket", immediately beneath the mouth. These limbs, 
although non-ambulatory, appear to be homologous with the 
five pairs of post-oral head limbs of Emeraldella (Fig. 6E). 
The latter has a single filamentous pre-oral flagellum that is 
apparently homologous with the short biramous "antenna" 
of Sanctacaris, In Emeraldella also, the post-oral head 
limbs are similar to the trunk limbs in being strongly ambu- 
latory as well as gnathobasic. 

On this interpretation, and in agreement with Delle Cave 
& Simonetta (1991), Sanctacaris is removed from the Chel- 
icerata and placed in Class Emeraldellacea within the revised 
superclass Trilobitoidea (Table ni,p. 24). Sanctacaris thus 
stands as a unique, relatively advanced, but apparently short- 
lived, sideline of Cambrian uniantennate evolution. 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 15 



FIG. 5. CAMBRIAN ARTHROPODS: WITH GNATHOBASIC LIMBS AND FILAMENTOUS 
PRE-ORAL APPENDAGES (variously from Gould (1989) and Briggs et al (1993) 


Evolutionary Pathways in Uniantennate Arthropods 

Plausible evolutionary pathways within uniantennate 
arthropods of the Cambrian period that led to more highly 
evolved trilobitoid and chelicerate faunas of the middle and 
late Paleozoic are summarized in Fig. 7 (p. 17). The chart 
embodies information provided in Table I, and figures 2, 3, 
5 & 6 especially. The degree of morphological evolution 
and specialization of feeding style is represented by four 
blocks or zones, proceeding along the X-axis, from the most 
primitive (pharyngeal feeding) on the left, through a narrow 

transitional band in the middle, to limb gnathobasic and limb 


masticatory feeding types on the right. Of these, the chelic- 
erate form on the extreme upper right is the most advanced. 
The Y-axis represents a generalized, rather than definitive, 
time scale. 

As noted previously, the most primitive and presumably 
ancestral uniantennate arthropod of the late Precambrian, 
Vendian, and Early Cambrian Periods was a member of the 
predatory and pharyngeal-feeding Anomalocarida, illus- 
trated on the lower left. These large-eyed animals possessed 
a short head (2-4 somites), and a multisegmented body with 
bilobate lateral pleurae or biramous ambulatory and 
respiratory paired appendages. In a cephalopodlike feeding 




AMPHIPACIFICA VOL. D. NO. 1 AUG. 31, 1995 


16 



FIG. 6. EXTERNAL MORPHOLOGY OF SANCTACARIS (modified from Briggs & Collins, 1988) 
A. Life-like Reconstruction. B. Dorsal View. C. Head region (MAG. X), D. Pre-oral appendage (X) 
E. (Inset). Head appendages of Emeraldella (ventral view) 

F. L/mu/us Left chelicera G. Cassubia Left Pre-oral Appendage. 


style, paired raptorial pre-oral head appendages apparently 
captured and transported food to the mouth region where it 
was masticated and ingested without post-oral limb assist- 
ance. Within the Anomalocarida per se . development of a 
benthic life style was accompanied by reduced segmentation 
but stronger armature, possibly partly fossorial in function, 
of the pre-oral raptorial limbs (e.g., 'm"Laggania" - type 
fossils (Table I) and in Cassubia Lendzion, 1977, centre 
line). 

Of the three proposed evolutionary offshots from the 
Anomalocarida, the epibenthic probosciferidans (on the left) 
developed a very specialized food capturing mechanism, 
similar in function to the hetercotyl arms of cephalopods, but 
found nowhere else among the arthropods. It consisted of 
horizontally opposing limbs fused together in a claw-like 


appendage that was activated by a flexible proboscoid ex- 
tension of the anterior head region. Its movements were pre- 
sumably triangulated and co-ordinated by widely set pairs of 
stalked compound eyes. The small size of this "proboscis", 
and lack of peribuccal or pharyngeal teeth, indicate that the 
prey organisms were very probably small and soft-bodied. 

Cladistic presentation of relationships of Tullimonst- 
rum by Beall (1991 ) may be a case of "bending the facts" to 
fit theoretical models. None of his cladograms provides 
close relationships between Tullimonstrum and other major 
invertebrate groups, and each cladogram contradicts rel- 
ationships depicted by the others. The "re-interpreted" ani- 
mal appears unfunctional (e. g., a vertical tail on a depressed 
trunk) and inconsistent with the taxonomic details of Rich- 
ardson (1966) and Johnson & Richardson ( 1969) that resulted 


AMPHIPACIFICA VOL. n. NO. 1 AUG. 31, 1995 17 



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no. 7. RELATIONSHIPS OF CAMBRUN UNIANTENNATE ATHROPODS 
BASED ON FEEDING MECHANISMS 






AMPHIPACIFICA VOL. n. NO. 1 AUG. 31, 1995 18 


from careful observations on numerous specimens. 

A more successful evolutionary experiment typifies the 
mostly benthic trilobitoid line to the right. In it, the pre-oral 
limb lost its raptorial function and became flagelliform, 
multi-segmented, and presumably mainly sensory and perhaps 
tactile in function. Simultaneously, the post-oral head and 
trunk limbs developed a linear gnathobasic endopod which, 
through various degrees of cephalization of anterior trunk 
segments, formed a masticatory feeding field of 2-5 pairs of 
post-oral head appendages. Remarkably, the species of 
Leanchoiliidea (including Acanthomeridion from Chengjiang 
deposits) sit squarely in the transitional zone of both pre- and 
post-oral limb evolution. Alalcomenaeus, having the most 
advanced, mono-filamentous pre-oral appendage, also has 
nearly fully gnathobasic post-oral appendages (Delle Cave 
& Simonetta, 1991). 

Of the flagellated trilobitoids with 3 post-oral head 
segments, the "spike-telsonic" group (centre right) encom- 
passed the Habelia subgroup having armoured processiferous 
bodies and short antenna. The associated Molaria, also 
having filamentous antenna and only three post-oral head 
segments, is an unlikely precursors of the chelicerates, as 
proposed by Delle Cave and Simonetta (1991, Chart II). 
Trilobitoideans withpygidial (non telsonic) abdomens (lower 
right) included narrow-bodied "idotheid" or "asellid" isopod- 
like forms such as Mollisonia and Urokodia that may have 
occupied algal substrates. They also included broad, flat- 
bodied, fossorial types with protective exoskeletal armour, 
leading to their only successful subgroup, the trilobites, that 
di versed in the later Paleozoic times. 

The trilobitoids include the Eraeraldellidacea that have 
5 post-oral head segments and a spike-like telson (upper 
right). The group here includes the aglaspids, thought to 
possess chelicerae prior to the work of Briggs et al (1978). 
Aglaspids "straddle" the Upper Cambrian- Lower Ordovician 
boundary. The Devonian Cheloniellon may be a distant 
descendent of the main line of Emeraldellidea. As mentioned 
above, a carnivorous form with paddle-like telson, Sancta- 
caris, is considered an early offshoot of this same line. This 
species has 5 distinct post-oral head segments, each with bi- 
ramous paired raptorial limbs. Sidneyia has no post-oral 
head limbs but the first four trunk limbs are uniramous 
(lacking gills), strongly gnathobasic and form, effectively, a 
post-oral masticatory field of four segments. Sidneyia is here 
regarded as a very early (relict) stage of cephalization of ant- 
erior trunk appendages, and had a separate origin (Fig. 7K). 

The most successful anomalocarid offshoot is here 
believed to be the Jianfengia- Yohoia line, to the upper right 
of Fig. 7. The post-oral head limbs, in the process of losing 
respiratory exopods, were already ambulatory and transitional 
in form. Although the pre-oral head limbs remained rapto- 
rial, their reduced size and segmentation and subcheliform 
appearance are plausible precursors to the fully chelicerate 
condition found in the most primitive arachnids, the mero- 
stomes, of the Lower Ordovician (upper right). However, 
the viability of this proposed evolutionary connection awaits 
discovery of a broadly flat-bodied fossil having transitional 


masticatory post-oral head and trunk limbs and a more 
clearly cheliform (rather than geniculate) pre-oral append- 
age. Triopus (Fig. 7P.1) may approach that predicted form 
but its appendages are poorly known. Chasmataspis (Fig. 
7P2) is the most primitive Lower Ordovician undoubted 
chelicerate, leading to the eurypterids. Although not 
completely understood (Bergstrom, 1979), Chasmataspis 
has 5 post-oral head segments and 12 trunk segments. The 
total is one more than the combined number of post-oral 
segments of the presumed ancestral Yohoia. 

The Euthycarcinoidea Enigma 

The enigmatic group of aquatic arthropods classified as 
Euthycarcinoidea, is based on a half-dozen limnic (?) species 
that existed from Carboniferous to Triassic time. Bergstrom 
(1979) summarized information on theTriassic generaEwr/iy- 
carcinus and Synaustrus, and Schram and Emerson (1991) 
utilized the upper Carboniferous genera Pieckoxerxes and 
Kottixerxes in developing their newly proposed Arthropod 
Pattern Theory (Fig. 8). The broad head shield is typically 
composed of 3 somites including an eye-bearing acron, an 
anterior procephalon with a single pair of filamentous anten- 
nae, and a posterior gnathocephalon bearing a set of mandi- 
ble-like appendages and on which the mouth opens ventrally . 
The broadened trunk is divided into an anterior (thoracic) 
region of diplo- or triplo- segments each bearing paired 
uniramous limbs, and a posterior narrower and limbless 
abdomen that terminates in a spikelike telson. 

According to Schram & Emerson (loc. cit.), the possession 
of uniramous limbs and diplosegments may link these animals 
to the ancestry of the terrestrial myriapods and hexapods 
(Uniramia of Manton, 1972). On the other hand, the overall 
appearance of euthycarcinoideans is grossly similar to some 
uniantennate arthropods having 3-6 head segments, and 
filamentous pre-oral limbs, e.g., Leanchoilia, Habelia, and 
Emeraldella. However, unlike the uniantennates, the trunk 
endopods are filamentous, multisegmented, and lack rapto- 
rial spines, gnathobases, and/or terminal claws. The leg seg- 
ments bear slender posterior marginal spines that are possi- 
bly of both natatory and respiratory support function, and in 
that respect resemble the exopods of some uniantennate 
arthropods (e.g., of Trilobitoidea). 

The Lower Cambrian Chengjiang fossil deposits in 
Yunnan region, South China, discovered in 1984, contain a 
number of very primitive arthropods yet imperfectly known, 
and mostly not included here. However, one of these, 
Fuxianhuia protensa Hou, 1987b, is remarkably similar in 
overall form to the euthycarcinoideans (above, and figs. 8A, 
9) as detailed recently by Chen et al. (1995) (Fig. 8 A-H). The 
body consists of a short, broad, head shield and an elongate 
trunk region. The latter is divided into a thorax of 17 broad, 
depressed, limb-bearing segments, and an abdomen of 14 
narrower and more cylindrical, legless segments, the last 
bearing a prominent telson spine. The head bears an anterior 
pair of large stalked eyes, a pair of filamentous pre-oral 
appendages (antennules) on somite 2 and, ventrally on 


AMPHIPACIFICA VOL. U. NO. 1 AUG. 31. 1995 19 


anteroveniral eye-bearing 
plate ederite 





FIG. 8. EUTHYCARCINOIDEA: Fuxianhuia protensa Hou, 1987 (Middle Cambrian) 
A. Dorsal reconstruction Head shield B., C. ventral reconstr. D. dorsal reconstr. 

E. Sutehelate head appendage F. Abdomen, ventral G. Abdomen (ventral X. 1987; 
showily limbs) H. Pieckoxerxes piekoae K. Kottixerxes glotiosus (A. B - after Hou. 
D-G (after Chen et al, 1995) H, L. (after Schram & Emerson, 1991). 

J, K, Euthycarcinus Aerr/m (after Bergstrdm, 1979), 



AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 20 


somite 3, a pair of subchelate raptorial limbs, presumably 
arising on either of side of the mouth. These superficially 
resemble the raptorial head limbs of the uniantennate arthro- 
pod Cheloniellon, the raptorial maxillae of remipede crus- 
taceans, and the raptorial first thoracic limbs of belostomatid 
hemipteran insects. However, they are unlike the paired 
palpless mandiblelike structure of the mouth region ascribed 
to a few specimens of Euthycarcinus (Bergstrom, 1979). 

In other details, however, the similarity of Fuxianhuia 
to euthycarcinoideans is remarkably close. The trunk limbs 
are biramous, with thin plate-like exopods, but the endopods 
are cylindrical, multisegmented, and lack terminal claws. 
These endopods are also similar to the multisegmented, 
basally shafted rami of larval skaracarids of the Cambrian 
"Orsten" fauna (Fig. 9, part). The limbless abdomen is found 
elsewhere in most maxillopodan crustaceans (e.g., several 
Skaracarida, Cirripedia, Copepoda, etc., and the 
Cephalocarida) as well as some phyllocaridans and phyllopod 
biantennates. The incomplete basal fusion of the trunk 
exopods and endopods is reminiscent of the lateral lobe-like 
paired flaps or limbs of the primitive dicephalosomatid 
uniantennates. Modem aquatic predators with "jacknife" 
raptorial limbs (above) are all free-swimming pelagic preda- 
tors, perhaps indicating a similar life style in euthycarcinids. 

In summary, Fuxianhuia bears some similarity to nearly 
every major group of arthropods of the Lower and Middle 
Cambrian Period but does not conform completely with any . 
In the very primitive structure of his head and locomotory 
limbs, and multi- segmented body, it is close to a model 
arthropod ancestral type (e.g., of Snodgrass, 1956). How- 
ever, the presence of two pairs of pre-oral head limbs, the 
first of which is filamentous and the second raptorial, is 
similar to the situation in crustaceans and some phyllocaridans, 
and thus essentially biantennate. This feature, along with the 
multisegmented, elawless endopods of the thoracic region, 
justify its inclusion within the class Euthycarcinoidea. Its 
other members are of more recent geological age, but 
sufficiently distinct to justify erection of the primitive sub- 
class Fuxianhuiacea (Table IV, p. 27). 

Evolutionary Relationships in Aquatic Biantennates 

A recapitulation of plausible evolutionary pathways 
within early aquatic biantennate arthropods is sketched in 
Fig. 9. On the left of the chart are connectives for two genera 
of skaracarid crustacean larval forms, a phosphotocopine 
ostracod, and a thecostracan cyprid, that represent the primi- 
tive evolutionary phases of skaracarid, ostracod and 
cirripedian maxillopodans of Cambrian times. Their primi- 
tive character states included the shaftlike form of the basal 
portion of the post-oral head limb endopods, the unbossed 
condition of their ramal spines and setae, and the multi- 
segmented rami that are found variously in early naupliar 
stages of Copepoda, Cirripedia, and other extant maxillopod- 
an crustacean subgroups. The systematics and evolutionary 
history of maxillopodan crustaceans are relatively well known 
(e.g., in Schram, 1986), and are not discussed further here. 


In the centre are the euthycarcinoideans of which 
Fuxianhuia from the Lower Cambrian is here designated the 
the most primitive member. The Upper Carboniferous and 
Triassic members are shorter-bodied, with diplo- and triplo- 
trunk segments, uniramus limbs, and may be ancestral to 
groups with the Myriapoda. However, further evidence from 
Silurian and Devonian representatives is needed to clarify 
such a phylogeny. 

To the centre right are connectives between the three 
subclasses of biantennates recognized here within a revised 
and restricted definition of Latreille's original crustacean 
class Phyllopoda (p. 26). These Cambrian groups resemble 
extant branchiopodan and leptostracan crustaceans, at least 
superficially, and may have had a late Precambiian or 
Vendian common ancestor. The branchiocarids and 
odaraiatids were regarded as unique arthropods and/or crus- 
taceans by Briggs (1976, 1981). However, they differ from 
true crustaceans in the 3- segmented head structure (lack of 
clearly defined maxillae and maxillary segments) and the 
carapace is mandibular rather than maxillary in origin. 
Although Schram (1986), following Briggs (1978), assigned 
the Canadaspida to Malacostracan subclass Phyllocarida, 
Dahl (1984, 1987) convincingly demonstrated primary dif- 
ferences of tagmatization, total number of body segments, 
position and form of the presumed mandible, limb structure 
and other anomalous features that, under existing defini- 
tions, remove the Canadaspida from the Phyllocarida, and 
the true Crustacea. 

In Fig. 9, lower right, are the marrellomorphs. These 
represent one of the few aquatic biantennate arthropods with 
qualifications for direct ancestry to the myriapods and hexa- 
pods, its leg features postulated by Kukalova-Peck (1992). 
Thus, marrellomorphs are biantennate and the head limbs 
possibly mandibulate, but not ambulatory-gnathobasic. They 
are mainly benthic in life style and the anterior limbs are 
apparently double-clawed, suited to walking or crawling 
over firm substrates. They also possess similar body 
tagmatization and limb structure, and the telson is minute or 
lacking. The leglike maxillary and labial palps of 
an Upper Carboniferous monuran wingless insect (Fig. 9) 
are remarkably similar in form to the endopods of the 
ambulatory head limbs of the Devonian marrellomorphs 
Mimetaster and Vachonisia (Stiirmer & Bergstrom, 1976). 
Loss of the second head segment and its antennalike pre-oral 
limbs in myriapods and hexapods accords with overall 
evolutionary trend to reduction of limbs and accessory lobes 
that accompany a shift from aquatic to terrestrial life style. 
In air, gravitational effects on limb structure are more signifi- 
cant; two pairs of sensory limbs would thus appear to be 
mechanically unwieldy and functionally unnecessary. 

Phylogenetic Tree of the Arthropoda 

An annotated classification of uniantennate and 
biantennate arthropods is presented in Tables III (p. 25) and 
IV (p. 27) respectively, the number of higher categories of 
which are summarized in Table V (p. 29). Hypothetical 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 21 



FIG. 9. PHYLETIC LINKAGES WITHIN BI ANTENNATE ARTHROPODS S 2 

OF THE PALEOZOIC ERA 


relationships of the major genera of the Cambrian Period to 

each other and to other major groups of arthropods over the 
600+ million year geological and evolutionary time scale are 
summarized in the accompanying chart (Fig. 10, p. 23). 

Phyletic relationships may be presented in a number of 

graphical ways, including cladograms (e.g. Briggs & Fortey 


1989), following an earlier attempt by Briggs (1983). Those 
authors (1989) utilized 26 characters and corresponding 
character states in deriving an arrangement in which the 
biantennate branchiopods clustered near the base, the 
trilobites at the advanced end, and various trilobitoideans 
and arachnids at intermediate levels of the evolutionary 





AMPHIPACMCA VOL. 11. NO. 1 AUG. 31, 1995 22 


scale. Whereas this scheme has an overall plausibility, it is 
limited in detail by the omission of dicephalosomatid arthro- 
pods or other related outgroup taxon, by other possibilities in 
the ordering of some character states, and by weaknesses 
inherent in cladistic analyses generally (see Gosliner and 
Ghiseln, 1984). 

In view of limitations of cladistic methodology at this 
stage of knowledge, the writer finds merit in modifications 
of the simple phyletic tree arrangements of Delle Cave & 
Simonetta (1991), for various early arthropod subgroups, as 
outlined here in Fig. 10. The hypothetical " tree" com- 
mences somewhere within late Precambrian times, in con- 
formity with the views of Dzik & Knimbiegel (1989). Thus, 
representatives of tardigrade and onychophoran pararthropods 
and both uniantennate and biantennate arthropods were 
already present in the earliest (Lower Cambrian) fossil 
deposits (Dzik &Lendzion, 1988). Also, protarthropods (e.g 
Xenusia) and some antennognath arthropods (e.g., Spriggina, 
Praecambridium) are also known from Ediacrian and V end- 
ian fossil deposits (Delle Cave & Simonetta, 1991). 

The earliest and morphologically most primitive 
uniantennulate subgroup of Cambrian times is here consid- 
ered to be the dicephalosomatids (p. 25). The primitive ano- 
malocarids did not suri ve the Cambrian and the more advanced 
probosciferans lasted only until the Upper Carboniferous. 
The Yohoiida, possibly on a direct ancestral line with the 
chelicerates, also became extinct in the Cambrian. Not yet 
discovered, however, is a theoretical Cambrian fossil form 
having a 6-segmented head, transitional post-oral mastica- 
tory limbs, and fully cheliceriform pre-oral appendages that 
might directly link the group with the chasmataspids and 
primitive aquatic arachnids of Ordovician and later periods. 
Of the aquatic merostomes, the eurypterids diversified dur- 
ing the mid Paleozoic but became extinct prior to the 
Mesozoic, and few relict limulids are the only modem 
survivors of those primitive aquatic chelicerates. 

The Trilobitoidea embodied various combinations of 
head and trunk segments having filiform, sensory pre-oral 
appendages and raptorial, gnathobasic, post-oral feeding 
and ambulatory limbs. Several of these, including early 
trilobites (e.g., olenellids) apparently became extinct during 
the Cambrian, although the Emeraldellidea persisted until 
the Devonian (e.g., Chelionellon). The more advanced 
trilobites became the single most speciose and diverse group 
of aquatic uniantennates during the early Paleozoic. They 
apparently survived longer than any other other arthropod 
group having only 4 head segments, but were gone by the 
beginning of the Mesozoic. 

The paleohistory of the biantennates is less clear. Prim- 
itive biantennates, the euthycarcinoids, marrellomorphs and 
phyllopods occurred, even abundantly, in the Cambrian. 
However, the inarrellomophs survived only until the Upper 
Paleozoic, and the euthycarcinoids to the Triassic. As noted 
on page 1 8, the marrellomorphs provide a plausible (but not 
confirmed) aquatic ancestor to the terrestrial myriapods and 
hexapods whose fossil records commenced in the lower 
Devonian and upper Silurian periods. Kukalova-Peck (1992) 


has provided convincing evidence that the myriapod and 

hexapods could not have originated from the Xenusian- 

onycophoran line of "uniramians", a conclusion supported 
by the present study. 

The fossil record of early cmstaceans is uneven, but 
little doubt exists, especially as result of remarkable new 
micro-fossils in the Swedish ’Orsten’ deposits, revealed by 
Walossek & Muller (1989), that the maxillopodans were a 
very diverse biantennate group by Middle and Upper Cam- 
brian times. Maxillopodans continued to exploit aquatic 
niches and food resources in which small size, free-swim- 
ming metamorphic developmental stages, and filter-feeding 
mechanisms are advantageous. The somewhat larger 
Branchiopoda, by developing a resting egg stage, have 
managed to survive, mainly in temporary freshwater habi- 
tats, over a comparable time frame. Their non-palpar 
mandible, even in early naupliar stages (Sanders, 1963), may 
indicate an early link with the Phyllopoda. There is little 
basis for a direct phyletic link with the trilobitoideans, as 
studied by Hessler & Newman (1975). 

With respect to the Cephalocarida and the Remipedia, 
crustacean classes discovered only during the later half of 
this century, their body and limb structures are more primitive 
than most other maxillopodans, and certainly the malacost- 
. racans (Schram, 1986). Despite their problematical late 
Paleozoic (or non-existant) fossil records, an early Paleozoic 
origin for both groups is a reasonable expectation. 

The Malacostraca may be considered the dominant and 
most diverse crustacean class of Recent times (Bousfield & 
Conlan, 1990). Transfer of the orders Canadaspida and 
Branchiocarida from the Crustacea to the phyllopod Bi- 
antennata (p. 25), leaves the Upper Devonian protoglyphaeid 
reptantian Palaeopalaemon newberryi as the earliest con- 
firmed malaeostracan fossil record (Schram, 1986). How- 
ever, the relatively plesiomorphic body segmentation and 
limb structure of the Leptostraca (sensu strictu), as well as 
the Hoplocarida and Syncarida, would suggest a somewhat 
earlier beginning for the malacostracans, possibly during the 
Silurian or late Ordovician. 

THE CAMBRIAN ARTHROPOD FAUNA: EVOLU- 
TIONARY TRENDS, 

Early trends in the direction of morphological and be- 
havioural evolution in arthropods, revealed by Burgess Shale 
and other Cambrian faunal assemblages, are summarized as 
follows: 

(1) Within uniantennate arthropods, the ancestral pharyn- 
geal and peribuccal feeding methodology was replaced by a 
masticatory assemblage of post-oral gnathobasic limbs of 
the head region. The taxonomic series of Anomalocaris, 
Leanchoilia and Emeraldella represents this transformat- 
ional process. 

(2) Also within the uniantennates, the primitively large 
raptorial food-gathering limbs of the pre-oral head region 
gave rise to short, paired cheliform and chiefly masticatory 
appendages within the higher (terrestrial) Chelicerata. The 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 23 



-LOG T 1 

M E 

LO 

o 

LO 


CO 

o 

CM 

to 

u> 


SCALE 


(M. Y. B. P.) 


o 



c.|mesoz 

FIG. 10. 


U. PAL. L. PAL CAMBRIAN 

PHYLOGENETIC TREE OF THE ARTHROPODA 


PRECAMBR. 


no. 10. PHYLOGENETIC TREE OF THE ARTHROPODA. EMPHASIZING THE MIDDLE CAMBRIAN FAUNA 

(Based parti}' «■ Schram (1986) and Boosfield & Coalan (1990) 




AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 24 


taxonomic sequence of Artoma/ocam, Yohoia, Chasmataspis, 

and the Scorpionida illustrates this evolutionary sequence. 

(3) Other types of pre-oral limb development that involved 
an opposing limb raptorial mechanism on the one hand, and 
a filamentous sensory structure on the other, did not survive 
the close of the Paleozoic Era. 

(4) The cephalization, or incorporation of masticatory limbs 
of anterior trunk segments into the head shield, of both uni- 
and bi-antennate arthropods, proceeded most rapidly during 
the Cambrian Period. Such a rapid evolutionary process in 
major taxonomic features may prove to be a direct example 
of punctuated equilibrium proposed by Eldridge & Gould 
(1972). However, few aquatic taxa with only 2-4 head 
somites (e.g., a few Probosciferida, Marrellomorpha) sur- 
vived beyond the Cambrian, although the euthycarcinoids 
persisted until the Triassic; some with five somites (e.g., 
Trilobita) reached the late Paleozoic; whereas groups with 6- 
7 head somites (e.g. Crustacea, Chelicerata) extended into 
Mesozoic and Recent times. 

(5) Primitively shaftlike and elongate trunk limbs became 
increasingly distinctly segmented, chitinized, and shortened, 
especially in benthic forms. A series of forms within the 
crustacean order Skaracarida (e.g. Data, Bredocaris, and 
Oleandocaris), the phosphatocopine ostracods, and the 
naupliar-metanaupliar stages of other maxillopodan 
crustaceans, illustrate such transformation. 

(6) The dorsal shield arises from the first head segment (pre- 
oral carapace) in primitive, pharyngeal -feeding arthropods. 
In more advanced, limb-masticatory arthropods (e.g., mandib- 
ulates) the carapace (secondarily bivalved) arises from the 
posterior segment of the head shield that is mandibular in 
phyllopods and typically maxillary in crustaceans. 

(7) With respect to the natatory function of limbs, swimming 
appendages occur in both post-oral head and trunkregions of 
very early uniantennates, and larval stages of more advanced 
arthropods. Coincident with tagmatization of the trunk into 
thorax and abdomen, and the "cephalization" of feeding 
limbs in higher taxa, swimming, and respiratory, functions 
shifted posteriorly from head to thorax and finally to abdo- 
men, as in stomatopods, isopods, and other Malacostraca. 

(8) Evolution of the terrestrial myriapods and hexapods from 
presumed aquatic ancestors apparently involved loss of the 
second pre-oral head segment and its antennate appendages. 
In the aquatic environment, those limbs are functionally 
sensory (see Callahan, 1979), locomotory, or even food 
gathering. In the terrestrial environment, such limbs 
presumably became duplicative and mechanically unwieldy, 
and followed into oblivion the original prothoracic wings of 
insects. Similarly, in peracaridan crustaceans that have 
become secondarily terrestrial (e.g., talitrid amphipods, 
oniscoidean isopods), one of the sensory antennal pairs (first, 
antennules) has become very much reduced or vestigial, with 
only one pair (second, antennal) remaining effectively 
functional. In similar vein, an alternative functional evolution 


of the head appendages of myriapods and hexapods would 

countenance die fusion of the first pre-oral limbs to the 
labrum to form the clypeo-lahrum, and the second pair of 
head appendages, equivalent to the second antennae of 
crustaceans, have become the monofilamentous antennae of 
the hexapods. However, embryological and/or paleohistorical 
(fossil) evidence for such a proposal has not yet been 
demonstrated. 

In summary, in the most successful arthropod groups of 
modem times, the head shield encompasses anterior limbs of 
the primordial tmnk region, limbs that assist in food capture 
and mastication. Body tagmatization has become pro- 
nounced, and swimming, ambulatory and respiratory func- 
tions are relegated increasingly to thoracic and abdominal 
limbs (see also Schram, 1986). In higher cmstaceans 
(malacostracans), thoracic limbs have become uniramous, 
cheliform and versatile, and the antennules secondarily bi- or 
tri-ramous and sensory. In higher arachnids, however (e.g. , 
pedipalpids and phalangids), the prosomal limb gnathobases 
have become secondarily lost, but feeding mechanisms 
remain primitive in the retention of chelicerate pre-oral 
limbs and a suctorial pharynx. In tracheates, the exopods of 
trunk limbs have been lost. In hexapods, the abdominal 
limbs have become vestigial or lost entirely, and exites of 
limbs have secondarily become gills and/or trachaeae in the 
abdomen, and trachaeae and/or wings in the thorax (see 
Kukalova-Peck, 1987,1 992). Such fundamental morpho- 
logical changes in arthropod body form have unquestionably 
contributed vitally to the ability of modem groups to utilize 
the diverse organic and plant-related food resources that 
have evolved mainly in terrestrial habitats, and mainly since 
the late Paleozoic Era. 

Source references for taxonomic andclassificatory names 
and time-scale occurrences in following Tables III-V are: 
E. L. Smith - unpublished MS "Atlas of Insect Morphology"; 
L. Stprmer (1959) - in Treatise on Invertebrate Paleontology ; 
J Bergstrom (1979) - "Morphology of Fossil Arthropods"; S. 
J. Gould (1989) - "Wonderful Life" & source materials; 
D.E.G. Briggs et al. (1993) - "The Burgess Shale fauna" and 
source material; L. Delle Cave & A. M. Simonetta (1991)- 
"Early Palaeozoic Arthropods"; T. Savory (1964) - "Arach- 
nids"; F. R. Schram (1986) - "Crustacea"; and numerous 
other source papers inducting arthropod sections in "Synop- 
sis and Classification of Living organisms", McGraw Hill, 
1982. 

A database for analysis of the paleohistorical occurence 
of major taxonomic groups is given in Table V (p. 28). Some 
taxonomic names, especially those relatively recently pub- 
lished or not sufficiently well described (e.g., Wapria Walcott, 
1912) have been omitted from the lists and the analysis. A 
complete bibliography of citations of taxonomic names is 
not included in the references here, but may be found in the 
Zoological Record or other basic reference texts for the taxa, 
author names and dates concerned. 


AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 25 


TABLE ni. SUGGESTED NATURAL CLASSIFICATION OF AQUATIC, ESPECIALLY EARLY 
PALEOZOIC, ARTHROPODA BASED ON FOOD-GATHERING AND FEEDING MECHANISMS. 


PHYLUM ARTHROPODA 

I. INFRAPHYLUM UNIANTENNATA, new name (= MANDIBULOPODA E. L. Smith ’Atlas ”) 
One pair of positionally and embryonically pre-oral head limbs; trunk limbs often gnathobasic. 


tSUPERCLASS DICEPHALOSOMATA Sharov, 1966 (L. Camb. - U. Carb) 

Pre-oral limbs raptorial, non cheliform, 4-14 segments; post-oral limbs non food-gathering; feeding pharyn- 
geal, assisted by pre-oral limbs; trunk 12+ segmented, pygidial?; limbs locomotory, respiratory; aquatic. 
tCLASS ANOMALOCARIDEA Raymond, 1935 (L. - M. Camb.) 

Pre-oral limbs paired, 7-14 segmented; 1-3 post-oral head segments; peribuccal teeth present. 
tSUBCLASS ANOMALOCARIDATA new (L. - M. Camb) 

Pre-oral limbs 1 1-14-segmented; 3 post-oral head segments; trunk limbs natatory 

tOrder Anomalocarida Raymond, 1935 (Anomalocaris Whiteaves, 1892; ?Hurdia Walcott 19121 
tSUBCLASS CASSUBIATA new (L. Camb) 

Pre-oral limbs 7-segmented; 1? post-oral head segment; anterior trunk limbs ambulatory? 
tOrder Cassubiida new {Cassubia Lendzion, 1977) 


tCLASS PROTOCHELICERATA Strmer, 1944, revised and restricted (L. - M. Camb.)0 

Pre-oral limbs paired, semi-chelicerate, 4-5 segmented; 3 pairs post-oral, biramous ambulatory head limbs. 
tSUBCLASS YOHOIIDACEA Henriksen 1928, new status (L. - M. Camb) 

Trunk limbs biramous, natatory, respiratory. 
tSuperorder Yohoiidea Henriksen 1928 
tOrder Jianfengiida new (Jianfengia Hou, 1987) (L. Camb) 
tOrder Yohoiida Henriksen 1928 (Yohoia Walcott, 1912) (M. Camb) 


tCLASS PROBOSCIFERIDEA Sharov, 1966 emend (M. Camb - U. Carb) 

Pre-oral limbs fused to clawlike (14- segmented) jaws on anterior proboscis; post-oral head segments and 
peribuccal teeth lacking. 


tSUBCLASS OPABINIIDACEA Stprmer, 1944 (M. Camb) 

tOrder Opabiniida St0nner, 1944 (Opabinia Walcott, 1912-, ?Kerygmachela Conway Morris etaK 1987) 
tSUBCLASS TULLIMONSTRIDEA E. L. Smith "Atlas" (U. Carb) 
tOrder TuUimonstrida (Tullimonstrum Richardson, 1966) 


tSUPERCLASS TRILOBITOMORPHA Stprmer, 1944, restricted status (L. Camb. - M. Perm.) 

Pre-oral limbs filamentous, non raptorial; post-oral head limbs and trunk limbs normally biramous, 
endopods modified for food-gathering and/or feeding. 

tCLASS (SUBCLASS) LEANCHOILIIDACEA Raymond, 1953, new status (L. - U. Camb.) 

2-3 pairs post-oral, spinose (or weakly gnathobasic) transitional head limbs; trunk limb endopods 
transitional; telson large. 

tSuperorder Leanchofliidea Raymond, 1935 

Head with 2 post-oral segments; pre-oral limbs multi-flagellate; eyes lacking. 
tOrder LeanchoBuda (L^awc/wi/ia Walcott, \9\2\ Acanthomeridion Hou, Chen &Lu, 1989 ) 
tSuperorder Alalcomenaeidea Simonetta, 1970 

Head with 3 post-oral segments; pre-oral limbs bi-flagellate or with accessory lobe; eyes present 
tOrder Actaeida {Actaeus Simonetta, 1970) 
tOrder Alalcomenaeida {Alalcomenaeus Simonetta, 1970; 

tCLASS (SUBCLASS) SIDNEYIDEA Walcott, 1911, new status (M. Camb.) 

Uc^ng post-oral head segment(s) or limbs; trunk not trilobate, limbs gnathobasic; telson flabellate 
tOrder Limulavida Walcott, 1911. {Sidney ia^^\co% 1911) (S«rarmcerc«^ - a larval stage?) 

tCLASS TRILOBITOIDEA Stprmer, 1955, restricted (L. Camb. - U. Perm.) 

3 pairs of post-oral gnathobasic, masticatory head limbs; trunk limbs biramous, endopods gnathobasic. 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 26 


fSUBCLASS BURGESSIDEA Walcott, 1912 (L. - M. Camb) 

Trunk lacking lateral pleurae, limbs biramous; tail region with spikelike telson. 
tOrder Burgessiida Walcott, 1912 {Burgessia Walcott, 1912) 

tOrder Molariida Walcott, 1912 {Molaria Walcott, 1912; Emeraldoides Simonetta, 1964) 
fOrder Habeliida Simonetta & delle Cave 1972 {Habelia Walcott, 1912; Thelxiopa; Economocaris) 

TRILOBITOIDEA INCERTAE SEDIS Tontoia Walcott, 1912. Nathorstia Walcott, \9\2\Retifacies Hou, 
Chen & Lu, 1989; Koumaia Hou, 1987; Rhombicalvaria. Hou, 1987; Helmetia Walcott, \9\lMollisonia 
Walcott, \9\2\Urokodia Hou, Chen & Lu, 1989; Corcorania Jell, 1980; Serracaris Briggs, 1978? 
tSUBCLASS TRILOBITA Walch, 1771 (L. Camb - U. Perm) 

Trunk segments typically with lateral pleurae (trilobate); tail region pygidial. 
tSuperorder Eotrilobitacea Whittington, 1977 (L. - M. Camb) 

tOrder Nectaspida Raymond, 1920 {Naraoia Walcott, 1912) (Inch Liwia & Tegopelte, L. Camb) 
tSuperorder Trilobitacea Walch 1771 (L. Camb - M. Perm) 
tOrder Agnostida Kobayashi 1935 
tOrder Redlichiida Richter, 1933 
tOrder Corynexochida Kobayashi, 1935 
tOrder Ptychopariida Swinnerton 1915 
tOrder Phacopida Salter, 1964 
tOrder Lichida Moore, 1959 
tOrder Odontopleurida Whittington, 1959 

tCLASS EMERALDELLIDEA Raymond, 1935 (M. Camb. - L. Dev.) 

5 pairs of post-oral, gnathobasic, masticatory head limbs; trunk limbs biramous, endopods ambulatory. 

tSUBCLASS SANCTICARIDEA E. L. Smith "Atlas" (M. Camb) 

Pre-oral limb biramous; post-oral head limbs raptorial, unlike ambulatory trunk limbs; telson flabellate. 
tOrder Sanctacarida E. L. Smith "Atlas" {Sanctacaris Briggs & Collins, 1988 [=Utahcaris orion Con- 
way Morris & Robison, 1988]). 

tSUBCLASS EMERALDELLACEA Raymond, 1935 (M. Camb - L. Dev) 

Pre-oral limb uniramous, filiform; post-oral head and trunk limbs ambulatory and raptorial; telson a spike 
tOrder Emeraldellida Simonetta & Della Cave, 1975, revised {Emeraldella Walcott, 1912) 
tOrder Cheloniellonida Brioli, 1933 {Cheloniellon Broili, 1932) (L. Dev) 
tOrder Aglaspida (Walcott, 1911) {Aglaspis Hall, 1862, revised Briggs et al, 1978) (L. Ord) 

Inclusions: Aglaspella, Beckwithia, Palaeomerus; Borchgrevinkium; Palaeoniscus, Kodymirus? 
Strabops? 

SUPERCLASS CHELICERATA Heymons 1901 (L. Ord - R) 

Pre-oral limb chelicerate, 3- (occasionally 2- or 4-) segmented; 5 (6) pairs of uniramous post-oral 
head limbs; trunk limbs uniramous, respiratory. 

CLASS MEROSTOMATA Dana, 1852 (L. Ord - R) 

Post-oral head limbs gnathobasic, first pair undifferentiated; trunk limbs reduced to book gills; aquatic. 

SUBCLASS XIPHOSURA Latreille 1802 (L. Ord -R) 

Pre- and post-abdomen strongly differentiated; one pair of compound eyes. 

Superorder Chasmataspididea Caster & Brooks, 1956, revised status (L. Ord - Dev) 

Post-abdomen 9-segmented; pre-abdomen 3-segmented? 

Order Chasmataspidida Caster & Brooks, 1950 (L. Ord-Sil) (Chasmataspis, Pseudoniscus) 

Order Diploaspidida Caster & Brooks, 1956 revised status (Dev) {Diploaspis, Heteroaspis) 
Superorder Xiphosuridea Latreille, 1802 (U. Sil. - R) 

Post-abdomen 1 -3-segmented; pre-abdomen 7(8)-segmented. 
tOrder Triopida Packard, 1886 (L. Ord) {Triopus ) 

tOrder Synxiphosurina Packard, 1886 (inch Weinbergina) (6 pairs post-oral head limbs) 

Order Limulina Richter & Richter, 1929 (Carb - R) {Limulus L. 1787; + Euproops (Carb)) 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 27 


fSUBCLASS EURYPTERIDA Burmeister, 1843 (L. Ord - Perm) 

Pre and post-abdomen not strongly demarcated; 2 pairs compound eyes 
tOrder Eurypterida Burmeister, 1843 (Eurypterus) 
tOrder Pterygota Clarke & Rudemann, 1912 

CLASS ARACHNIDA Lamarck 1801 (Ord. - R) 

Post-oral head limbs (secondarily) non-gnathobasic, first often differentiated as pedipalps; feeding 
chelicerate; anterior trunk limbs forming book lungs or lacking; terrestrial 
SUBCLASS SCORPINIATA Latreille, 1817 (Sil - R) 

Order Scorpionida Latreille 1806 (Sil - R) 

SUBCLASS PEDIPALPATA Latreille 1906 (M. Dev - R) 

Order Palpigradida Thorell, 1881 (Jur - R) 

Order Schizomida Petrunkevitch, 1945 (U. Tert - R) 

Order Uropygida Thorell, 1882 (U. Carb - R) 

Order Amblypygida Thorell 1883 (U. Carb - R) 

Order Aranaea Clerck, 1757 (U. Carb - R) 
tOrder Trigonotarbita Petrunkevitch, 1949 (M. Dev - U. Carb) 

SUBCLASS PHALANGIATA Leach, 1915 (U. Carb - R) 

Order Solfugida Leach 1815 (U. Carb - R) 

Order Acarida Nitzsch 1818 (M. Dev - R) 

Order Ricinulida Thorell, 1 892 (U. Carb - R) 

Order Opilionida Sundevall 1833 (U. Carb - R) 

Order Pseudoscorpiooida Latreille, 1817 (Olig. - R) 

CLASS PYCNOGONIDA Latreille, 1910 (L. Dev - R) 

Post-oral head limbs non-gnathobasic, first differentiated as pedipalps; feeding pharyngeal, pre-oral 
limb assisted; aquatic. 

tSUBCLASS PALAEOPYCNOGONIDA E. L. Smith Atlas (L. Dev) 
tOrder Palaeoisopida Hedgepeth, 1978 (Palaeoisopus Broili, 1928) 
tOrder Palaeopantopoda Broili, 1930 (Palaeopantopus Broili, 1928) 

SUBCLASS PODOSOMATA Leach, 1813 (L. Dev - R) 

Order Pantopoda Gerstaeker, 1963 {Pycnogonum littorale L.) 


TABLE IV. SUGGESTED NATURAL CLASSIFICATION OF BUNTENNATE ARTHROPODS 

2. INFRAPHYLUM BIANTENNATA Bergstrom, 1979 revised (= MANDIBULATA Clairville, 1798) 

Head with acron and 2 pairs of positionally pre-oral limbs, 2nd pair embryonically post-oral, biramous- 3rd 
(when present) mandibulate; trunk limbs not gnathobasic. 


tSOTERCLASS EUTHYCARCINOMORPHA Handlirsch, 1914, revised status (L. Camb. - Trias) 
Head 2(3)-segmented; head shield not maxillary; trunk tagmatized; thoracic limbs primitively biramous 
endopods slender, multi-segmented, lacking terminal claws; abdomen limbless, with telson.. 


tCLASS EUTHYCARCINOIDEA Handlirsch, 1914 (L. Camb - U. Trias) 

With the characters of the superclass. 
tSUBCLASS FUXIANHUIATA new (L. Camb) 

multi-segmented, segments simple, each with one pair of biramous limbs; telson short. 
tOrder Fuxianhuiida new (Fuxianhuia protensa Hou, 1987) 

INCERTA SEDIS: Chengjiangocaris longiformis Hou & Bergstiom, 1991. 
tSUBCLASS EUTHYCARCINATA Handlirsch, 1914. (U. Carb - Trias) 

Trunk with few (<20) diplo- and/or triplo- segments; trunk limbs uniramous, two per diplo- 
segment; telson elongate. 


tOrder Sottixeriformes Schram & Rolfe, 1982 (Pieckoxerxes piekoae Starobogatov, 1988) 
tOrder Euthycarciniformes Schram & Rolfe, 1982 (Kottixerxes gloriosus Starobogotov, 1988) 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 28 


fSUPERCLASS MARRELLOMORPHA Walcott, 1912, new status (M. Camb - L. Dev) 

Head 2-4- segmented; head shield spinose or bivalved, not maxillary; mandible, endopod leglike; trunk not 
tagmatized; trunk limbs undifferentiated, endopods strongly leglike, ambulatory, exceeds narrowly lamellate. 

tCLASS MARRELLIDEA Walcott, 1912 (M. Camb - L. Dev) 

Head 2-3 segmented; head shield with paired spines; telson minute. 
tSUBCLASS MARRELLATA Walcott, 1912 (M. Camb) 

Head 2-segmented; first post-oral head limbs antenna-like, 
t Order Marrellida Walcott, 1912 (Marre/la Walcott, 1912) 
tSUBCLASS MIMETASTERATA E. L. Smith "Atlas” (L. Dev) 

Head 3-segmented; first post-oral head limbs leg-like, 
tOrder Mimetasterida {Mimetaster Gurich, 1931) 

fCLASS ACERCOSTRACA Lehmann, 1955 (L. Dev) 

Head 4-segmented; head shield with carapace. 
tSUBCLASS VACHONISIATA E. L. Smith "Atlas" (L. Dev) 

Post-oral limbs 3 & 4 leglike, weakly gnathobasic. 
tOrder Vachonisiida new (Vachonisia Lehmann, 1955) 

tSUPERCLASS PHYLLOPODA Latreille, 1825 revised, restricted (M. Camb - L Ord) 

Head 3-segmented; head shield bivalved, not maxillary; mandible masticatory, not leglike or palpate; trunk 
15+ segmented, weakly tagmatized; endopods weakly leglike, exopods broadly lamellate (phyllopodous). 

tCLASS BRANCHIOCARroEA E. L. Smith "Atlas" (M. Camb) 

Head 3-segmented; trunk segments numerous (20+), with similar phyllopodous limbs. 
tSUBCLASS BRANCHIOCARATA E. L. Smith "Atlas" (M. Camb) 

First two pairs of head appendage prominent, 2nd pair cheliform?; carapace normal; tail region bifid. 
tOrder Branchiocarida E. L. Smith "Atlas" (Branchiocaris Briggs, 1976) 
tSUBCLASS ODARAIATA Simonetta & Delle Cave, 1975 (M. Camb) 

Pre-oral appendages minute, linear?; carapace tubular; tail region trifid. 
tOrder Odaraiida Simonetta & Delle Cave, 1975 {Odaraia Walcott, 1912) 

tCLASS (SUBCLASS) CANADASPIDIDEA Novoshilov, 1960 (M. Camb - L, Ord) 

Head appearing indistinctly 5-segmented, posterior 2 pairs of limbs similar to trunk limbs; trunk 
15-segmented, posterior 7 segments lacking paired appendages. 

tOrder Canadaspidida (Canadaspis Novoshilov, 1960; Perspicaris Briggs, l911\?Rhebachiella 
kinnekullensis Muller 1983 (larval stages) 

?Order Hymenostraca Rolfe, 1969 {Hymenocaris Salter, 1853) (M. Camb - L. Ord) 

SUPERCLASS CRUSTACEA Pennant, 1777 (after Schram, 1986) (M. Camb - R) 

Head with pre-oral antenna and 4 post-oral limbs, first antennalike, 2-4 (including mandible) masticatory; 
head shield maxillary; trunk often tagmatized, limbs often differentiated, specialized; telson present. 

CLASS (SUBCLASS) REMIPEDU Yager, 1981 (M. Dev - R) 

tOrder Enantiopoda Birshtein, 1960 (Tesnusocaris Brooks, 1955) (M. Dev) 

Order Nectiopoda Schram, 1986 {SpeleonectesYdigQX, 1981) (R) 

CLASS BRANCHIOPODA Latreille, 1817 (L. Dev - R) 

SUBCLASS SARSOSTRACA Tasch, 1969 (M. Dev - R) 
tOrder Lipostraca Scourfield, 1926 (M. Dev) 

Order Anostraca Sars, 1867 (L. Dev - R) 

SUBCLASS CALMANOSTRACA Tasch, 1969 (M. Dev. - R) 

Order Notostraca Sars, 1867 (L. Dev - R) 


AMPHIPACIFICA VOL. II. NO. 1 AUG. 31, 1995 29 


Order Kazacharthraca Novozhilov, 1957 (L. Jur) 

Order Conchostraca Sars, 1867 (L. Dev - R) 

Order Cladocera Latreille, 1829 (Perm-R) 

CLASS (SUBCLASS) CEPHALOCARIDA Sanders. 1955 (R) 

Order Brachypoda Birshtein, 1960 (Hutchinsoniella Sanders, 1955) 

CLASS MAXILLOPODA Dahl, 1956 (L. Camb - R) 
tSUBCLASS SKARACARIDA Muller, 1983 (M. Camb - U. Camb)) 

Order Skaracarida Muller, 1983. Skara annulata Muller, 1983) (several other, mostly larval genera 
e.g., Dala, Walossekia, Oelandocaris, Bredocaris, 

SUBCLASS OSTRACODA Latreille, 1836 (L. Camb - R) 
fOrder Bradoriidae Matthew, 1902 

t Order Phosphatocopida K. J. Muller, 1964 (L. Camb. - L. Ord) 
tOrder Leperditicopida Scott, 1961 (U. Camb - U. Dev) 
fOrder Palaeocopida Henningsmoen, 1953 (L. Ord - Trias) 

Order Halocyprida Dana 1852 (Sil - R) 

Order Platycopida Sars 1866 (L. Ord - R) 

Order Cladocopida Sars 1866 (Ord - R) 

Order Myodicopida Sars, 1966 (Ord - R) 

Order Podocopida Sars, 1866 (Sil - R) 

SUBCLASS THECOSTRACA Gruvel, 1905 (M. Camb - R) 

Order Facetotecta Gruvel, 1905 
Order Rhizocephala F. Muller, 1862 
Order Ascothoracida LacazcrDuthiers, 1880 
Order Cirripedia Burmeister, 1834 (M. Camb - R) 

SUBCLASS TANTULOCARIDA Boxshall & Lincoln, 1983 (R) 

Order Tantulocaridida Boxshall & Lincoln, 1983 
SUBCLASS COPEPODA Milne-Edwards, 1840 (Cret - R) 

Order Calanoida Sars, 1903 
Order Harpacticoida Sars, 1903 
Order Cyclopoida Burmeister, 1834 
Order Misophrioida Gurney, 1933 
Order Monstrilloida Sars, 1903 

Order Siphonostomatoida Thorell, 1859 emend Sars 1918 
Order Poecilostomatoida Thorell 1 859 

SUBCLASS LINGULATULIDA Frolich, 1789 (=Pentastomatida Rudolphi 1819) (R) 

Order Cephalobaeniuda Heymons & Vitzthum, 1936 
Order Porocephalida Heymons & Vitzthem, 1936 

tCLASS (SUBCLASS) THYLACOCEPHALA Pinna, Arduini et al. 1982. (Camb? L. Sil - Cen) 
tOrder Concavicarida Briggs & Rolfe, 1983 (L. Sil - Cen) 
tOrder Conchyliocarida Secretan, 1983 (Camb? - Jur) 

CLASS MALACOSTRACA Latreille 1806 (Dev - R) 

SUBCLASS PHYLLOCARIDA Packard, 1879 emended (Dev - R) 
tOrder Archaeostraca Claus, 1888 
tOrder Hoplostraca Schram, 1973 
Order Leptostraca Claus, 1880 (see also Dahl, 1984) 

SUBCLASS HOPLOCARIDA Caiman 1904 (U. Dev - R) 
tOrder Aeschronectida Schram, 1969 (Carb) 
tOrder Palaeostomatopoda Brooks, 1955 (U. Dev - L. Carb) 

Order Stomatopoda Latreille, 1817 (Carb-R) 

SUBCLASS EUMALACOSTRACA Grobben, 1892 (modified from Schram, 1986) (U. Dev - R) 
Superorder Syncarida Packard, 1885 (U. Carb - R) 
tOrder Palaeocaridacea Brooks, 1962 


AMPHIPACinCA VOL. H. NO. 1 AUG. 31, 1995 30 


Order Anaspidacea Caiman, 1904 
Order Bathynellacea Chappuis, 1915 
Order Stygocaridacea Noodt ,1964 
fSuperorder Belotelsonidea Schram, 1981 
tSuperorder Waterstonellidea Schram, 1981 
fSuperorder Eocaridacea Brooks, 1962 
Superorder Thermosbaenacea Monod, 1927 
Superorder Mysidacea Boas, 1883 
Order Lophogastrida Boas, 1883 
fOrder Pygocephalomorpha Beurlen, 1930 
Order Mysida Boas 1883 
Superorder Amphipoda Latreille, 1916 
Superorder Hemicaridea Schram, 1981 emended 
Order Spelaeogriphacea Gordon, 1957 
Order Mictacea Bowman et al. 1985 
Order Cumacea Kroyer, 1846 
Order Tanaidacea Dana, 1853 
Superorder Isopoda Latreille, 1817 
Superorder Eucarida Caiman, 1904 
Order Euphausiacea Dana, 1862 
Order Amphionidacea Williamson, 1973 
Order Decapoda Latreille, 1803 

SUPERCLASS MYRIAPODA Latreille, 1796 (Sil - R) (Essentially terrestrial; not detailed here) 

Head with embryonic acron, pre-oral antenna, 5 post-oral pairs of masticatory limbs (1st post-oral embry- 
onic); trunk not tagmatized, with more than 20 pairs of ambulatory limbs, ending in telson. 

CLASS SYMPHYLA Ruder, 1880 (1 subclass) (Olig-R) 

CLASS CHILOPODA Latreille, 1802 (2 subclasses) (M. Dev - R) 

CLASS PAUROPODA Lubbock, 1866 (1 subclass) (R) 

CLASS DIPLOPODA Gervais, 1844 (3 subclasses) (Sil - R) 
fCLASS ARTHROPLEURIDEA Zittel, 1848 (1 subclass)(L. Dev - U. Carb) 

SUPERCLASS HEXAPODA (L. Dev. - R.) (Essentially terrestrial; not detailed here) 

Head with acron + pre-oral antenna, 4 post-oral pairs masticatory limbs (1st post-oral embryonic, 2nd mand- 
ibulate; trunk tagmatized; thorax with 3, abdomen with 11 (max.) pairs ambulatory limbs; telson embryonic. 
CLASS PARINSECTA (2 Subclasses: CoUembola, Protura) (L. Dev - R) 

CLASS INSECTA (2 Subclasses Entognatha, Ectognatha) (U. Carb - R). 


TABLE V. NUMBERS OF fflGHER ARTHROPOD TAXA SINCE CAMBRIAN TIMES. 




P 

E R I 

O 

D 



ARTHROPOD 

INFRAPHYLA 

I 

CAMBRIAN 

(545-495 mybp) 

II 

LATE PALEO- 
ZOIC 

(-300 mybp) 

ni 

TERTIARY- 
RECENT 
(0-30 mybp) 


IV 

TOTALS 


SPCL. CL. 

SBCL. 

SPCL. CL. 

SBCL. 

SPCL. CL. SBCL 

SPCL. 

CL. SBCL. 

UNIANTENNATA 

2 8 

11 

3 5 

8 

1 3 5 

3 

10 18 

BIANTENNATA 

4 6 

9 

5 11 

24 

3 12 24 

6 

18 34 

TOTAL 

ARTHROPODA 

6 14 

20 

8 16 

32 

4 15 29 

9 

28 52 


AMPHIPACIFICA VOL. H. NO. 1 AUG. 31, 1995 31 


Arthropod Diversity and Evolutionary Trends 

Table V summarizes (from Tables m & IV) the number 
of higher arthropod taxonomic categories, recognized here at 
superclass (SPCL), class (CL) and subclass (SBCL) levels, 
that are represented by known genera and species of the 
Cambrian, late Paleozoic and Tertiary-Recent Periods. 
Analysis of the changing numbers with geological time re- 
veals interesting and perhaps significant evolutionary trends . 

Despite the very great difference in numbers of species 
known for each of the three time-scale samplings (Cambrian 
~102 species; Late Paleozoic- ~10 "^-i-species; Tertiary-Re- 
cent — 10 ^ + species), the numbers of higher taxa are of 
comparable orders of magnitude for all categories. In the 
600-million-year time span since the presumed dawn of 
arthropod life (Ediacrian, Vendian), we here categorize only 

9 superclasses, 28 classes and 52 subclasses to encompass 
the entire known fauna, past and present, of well over one 
million described species (Table V, Col. IV, bottom row). 
Fully one- third of the early subclasses is known from only 1- 

10 species, a fact suggesting the likelihood of further new 
discoveries, at that level or higher, among incompletely 
described or totally new fossil material. Only one of the 9 
superclasses (Crustacea), one of the 28 classes (Maxillopoda) 
and only two of the 52 subclasses (Ostracoda, Thecostraca) 
have actually been recorded throughout this immense 
paleontological range. To this meager total we might add the 
Chelicerata but it is presently confirmed not earlier than 
Lower Ordovician. However, further analysis of Paleozoic 
fossil material is expected to extend the time range of extinct 
species forwards, and recent species (especially minute, 
soft-bodied forms), backwards in time. Thus, the morph- 
ologically primitive Remipedia and Cephalocarida may 
have originated during Cambrian times, despite their very 
limited or non-existent fossil records (see Hessler, 1984). 
Aquatic larval stages of some other classes of Crustacea and 
of the merostomatid uniantennates (e.g., phyllocarid and 
trilobite larvae, respectively), tend to recapitulate adult mor- 
phology of extinct, but related, Cambrian categories. 

Thus, by the Cambrian Period, 67 % (6/9) of the super- 
classes, but only -50% (14/28) of the classes and -38% (20/ 
52) of the subclasses had evolved. By the late Paleozoic, 
perhaps the heyday of arthropod evolution generally, nearly 
all (8/9) the superclasses, and -60% (16/28; and 32/52) of 
all classes and subclasses were represented. Today, however, 
scarcely half (4/9 and 15/28) the superclasses and classes 
persist, and the percentage of subclasses, 56% (29/52), has 
also dropped slightly. 

If trends are analysed according to infraphylum for 
each time interval, for the uniantennates the percentages 
were highest during the Cambrian, with 33% (2/6) of the 
superclasses, 57% (8/14) of the classes, and 55% (1 1/20) of 
the subclasses. However, the group decreased markedly in 
importance by the late Paleozoic (only 37% of superclasses, 
-3 1% of classes, and -25% of subclasses), and is lowest to- 

day (25% of superclasses, -20% of classes, and only -17% 


of subclasses). By contrast, the biantennates increased 
steadily from lowest values in the Cambrian (67% of super- 
classes, 43% of classes and 45% of subclasses), through the 
late Paleozoic (63% of superclasses, -70% of classes, and 
-67% of subclasses), to maximum dominance today (75% of 
superclasses, -80% of classes, and -83% of subclasses). 

These changes in relative numbers of the two arthropod 
infraphyla may reflect the impact of the evolution of vascular 
plants during Silurian-Devonian and later periods (Kukalova- 
Peck, 1987). That event provided an enormous new food 
resource in both aquatic and terrestrial environments. These 
nutrients could be exploited by the omnivorous aquatic 
crustaceans and terrestrial myriapods and hexapods by direct 
adaptation and diversification of feeding morphology and 
style (as in malacostracan crustaceans, and winged insects). 
By contrast, the uniantennates were more or less “locked 
into” their mainly carnivorous, and some detritivorous life 
styles; they could take only indirect advantage of this food 
resource, and only by developing new predatory morph- 
ologies and life styles, especially within the terrestrial 
environment. They are now a secondary part of the terrestrial, 
and a minute relict part of the aquatic, arthropod fauna. 

With respect to the level of arthropod disparity during 
Cambrian times, the positions of both Gould (1989) and 
proponents to the contrary (e.g., Ridley, 1993; Wills et al. 
1994) receive support from the present analysis. Thus, of 9 
"all-time" arthropod superclasses, 7 (including Chelicerata) 
were represented in Cambrian and Lower Ordovician fau- 
nas, but only 4 are represented in the Recent fauna. Espe- 
cially remarkable is the fact that Cambrian arthropods were 
entirely aquatic, and were represented by less than 100 
species from a very limited series of marine habitats. The 
two superclasses missing from the Cambrian record, the 
Myriapoda and the Hexapoda, are both essentially terres- 
trial. Thus, if only aquatic faunas are considered, the 
disparity level of Cambrian arthropods is more than 3 times 
greater (7 vs. 2 superclasses) than today. 

On the other hand, at class level, disparity levels are 
similar ( 14 vs. 15), and at subclass level, the Recent arthropod 
fauna is about 50% richer (29 vs. 20). Furthermore, all of 
the arthropod, or arthropodlike, species of the Burgess Shale, 
designated by Gould (1989) and Briggs et al. (1993) as new 
(or probably new) at phylum and/or infraphylum levels, can 
be adequately encompassed within existing class and/or 
superclass categories. 

Thus, it is concluded here that, during the entire evolu- 
tionary history of the Arthropoda, disparity levels were at or 
near maximum during the Cambrian Period. Such a high 
level, close to the starting point of the arthropod fossil rec- 
ord, is consistent with the probable correctness of the evol- 
utionary theory of punctuated equilibrium (Eldridge & Gould, 
1972). Since invertebrate faunas of early "explosive evolu- 
tionary" times were not described comprehensively until the 
early 20th century (e.g., Walcott (1912), and later), Charles 
Darwin (1859) may be excused for missing that part of the 
evolutionary story. 


AMPHIPACMCA VOL. II. NO. 1 AUG. 31, 1995 32 


REFERENCES 

Beall, B. S., 1991. The Tully Monster and a new approach 
to analyzing problematica. pp. 271 -285. jn Simonetta, 
A. M. and S. Conway Morris (eds). The early evolut- 
ion of Metazoa and the significance of problematic taxa. 
Cambridge Univ. Press, New York. 

Bergstrom, J., 1979. Morphology of Fossil Arthropods as 
a Guide to Phylogenetic Relationships. in_ Arthropod 
Phylogeny. A. P. Gupta, (ed). Van Nostrand. Rein- 
hold Co., New York. Sect. 1: 3-55. 

, 1986. Opabinia and Anomalocaris, unique 

Cambrian "Arthropods". Lethaia 19: 241-246. 

, 1987. The Cambrian Opabinia and Anomalo- 

caris. Lethaeia Seminar. Lethaia 20: 187-188. 

Borradaile, L. A., and F. A. Potts, 1941. The Invertebrata. 
2nd Edition. MacMillan, New York. 706 pp. 

Bousfield, E. L., 1987. Review of : Crustacea, by F. R. 
Schram (1986). Oxford University Press, New York, 
Oxford. 606 pp. in: Jour. Crust. Biol. 7(4): 781-182. 

, & K. E. Conlan, 1990. Malacostraca. The 

Crustacea. J. Green & W. Newman (eds.}.in: Encyclo- 
paedia Britannica. Macropaedia, Vol. 16: 840-859. 

Briggs, D. E. G., 1976. The arthropod Bra/ic/imcam, n. gen., 
Middle Cambrian, Burgess Shale, British Columbia. 
Geol. Surv. Can. Bull. 264:1-29. 

, 1978. The morphology, mode of life, and af- 
finities of Canadaspis perfecta (Crustacea, Phyllocar- 
ida). Middle Cambrian, Burgess Shale, British Columbia. 
Phil. Trans. Roy. Soc. London B 281: 439-487. 

, 1979. Anomalocaris, the largest known 

Cambrian arthropod. Palaeontology 22: 631-664. 

, 1981. The arthropod Odaraia a/afa Walcott, 

Middle Cambrian, Burgess Shale, British Columbia. 
Phil. Trans.' Roy. Soc., London B 291: 541-585. 

, 1983. Affinities and early evolution of the 

Crustacea: the evidence of the Cambrian fossils. la 
F. R. Schram (ed.) Crustacean Phylogeny, pp. 1-22. 
Balkema, Rotterdam. 

, & D. E. Collins, 1988. A Middle Cambrian 

chelicerate from Mount Stephen, British Columbia. 
Paleontology 31: 779-798, 6 figs. 

, D. H. Erwin, & F. J. Collins, 1993. The fos- 
sils of the Burgess Shale. Smiths. Inst. Press, Washing- 
ton: 256 pp., illustr. 

, & R. A. Fortey, 1989. The early radiation 

and relationships of the major arthropod groups. Science 
246: 241-243. 

, & M. A. Wills, 1992. Mor- 
phological Disparity in the Cambrian. Science 256: 
1570-1673. 

, & H. B. Whittington, 1985. Modes of Life 

of Arthropods from the Burgess Shale, British Colum- 
bia. Trans. Roy. Soc. Edinburgh 76:149-160. 

, 1987. The affinities 

of the Cambrian animals Anomalocaris and Opabinia, 


Lethaia 20: 1 85- 1 86. 

Bruton, D. L., 1981 . The arthropod Sidneyia inexpectans, 
Middle Cambrian, Burgess Shale, British Columbia. 
Phil. Trans. Roy. Soc., London B 295: 619-656. 

, and H. B. Whittington, 1983. Emeraldella 

andLeanchoilia, two arthropods from the Burgess Shale, 
Middle Cambrian, British Columbia. Phil. Trans. Roy. 
Soc. London B 300: 553-582. 

Callahan, P. S., 1979. Evolution of antennae, their sensil- 
lae, and the mechanism of scent detection in Arthrop- 
oda. pp. 259-298. in Arthropod Phylogeny. A. P. Gupta 
(ed.). Van Nostrand Reinhold Co., New York. 

Chen, J.-y,L.Ramskold, and G.-q. Zhou, 1994. Evidence 
for monophyly and arthropod affinity of Cambrian giant 
predators. Science 264: 1304-1308. 

, G. D. Edgecombe, L. Ramskold, G-q. Zhou, 

1995. Head segmentation in Early Cambrian Fuxianhuia : 
Implications for Arthropod Evolution. Science 268: 
1339-1343. 

Collins, D. H., 1987a. The great Anomalocaris mystery. 
Rotunda. Winter, 1986-87: 51-57. 

, 1987b. Life in the Cambrian Seas. Nature 

326 (6109): 127. 

, & D. M. Rudkin, 1981. Priscansermarinus 

bametti, a probable lepadomorph barnacle from the 
Middle Cambrian Burgess shale of British Columbia. 
Jour. Paleont. 55(5): 1006-1015. 

Conway Morris, S., 1986. The community structure of the 
Middle Cambrian phyllopod bed (Burgess Shale). 
Paleontology 29: 423-467. 

— , and H. B. Whittington, 1985. Fossils 

of the Burgess Shale. A national treasure in Yoho Nat- 
ional Park. Geological. Survey of Canada, Misc. Re- 
ports, 43: 1-31. 

, J. S. Peel, A. K.Higgins, N. J. Soper, & 

N. C. Davis, 1987. A Burgess shale-like fauna firom the 
Lower Cambrian of North Greenland. Nature, 326 
(6109): 181-183, 2 figs. 

, & R. A. Robison, 1988. More soft- 

bodied animals and algae from the Middle Cambrian of 
Utah and British Columbia. Paleont. Contr. Univ. Kan- 
sas. Paper No. 122. 48 pp, 32 figs. 

Dahl, E., 1984. The subclass Phyllocarida (Crustacea) and 
the status of some early fossils: a neontologists’ view. 
Vidensk. Meddr. dansk. naturh. Foren. 145: 61-76. 

, 1987. Critique of Schram’ s Phyllocarida con- 
cept. Vidensk. Meddr. dansk. naturh. Foren. 148: 75. 

Darwin, C., 1859. On the origin of species. London: John 
Murray. 

Delle Cave, L. & A. M. Simonetta, 1991. Early Palaeozoic 
Arthropods and problems of arthropod phylogeny: with 
some notes on taxa of doubtful affinities, pp. 189 - 244. 
in Simonetta & Conway Morris (eds.). The early evolu- 
tion of Metazoa and the significance of problematic taxa 
1991. Cambridge Univ. Press, London. 

Dzik, J., &G. Knimbiegel, 1989. The oldest ‘onychophoran’ 


AMPHIPACinCA VOL. H. NO. 1 AUG. 31, 1995 33 


Xenusion: a link connecting phyla? Lethaia 22: 1 69- 1 8 1 . 

, & K. Lendzion, 1988. The oldest arthropods 

of the East European platform. Lethaia 21: 29-38. 

Eldridge, N., & S. J. Gould, 1972. Punctuated Equilibrium: 
neo-Darwinian evolutionary mechanism. Scientific Am- 
erican 262(3): 38-38. 

Foote, M., & S. J. Gould, 1992. Cambrian and Recent mor- 
phological disparity. Science 258: 1916. 

Fortey, R. A., 1989. Review of : Wonderful Life: The Bur- 
gess Shale and the Nature of History, by S. J. Gould 
(1989). Norton, New York. 347 pp. 

Glenner, H. and J. T. Hoeg, 1995. Scanning electron micro- 
scopy of cypris larvae of Balanus amphitrite (Cirripedia: 
Thoracica: Balanomorpha). Jour. Crust. Biol. 15(3): 
523-536. 

Gosliner, T. M., &M. T. Ghiseln, 1984. Parallel evolution in 
opisthobranch gastropods and its implication for phylo- 
genetic methodology. Syst. Zool. 33(3): 255-274. 

Gould, S. J., 1989. Wonderful Life (The Burgess Shale 
and the Nature of History). Norton & Co., Inc., New 
York. 347 pp. 

, 1993. How to analyze Burgess Shale disparity 

a reply to Ridley. Paleobiology 19(4): 522-523. 

Hessler, R. R., 1984. Cephalocarida: living fossil without 
a fossil record. In N. E. Eldridge and S. M. Stanley, 
(eds.). Living fossils, pp. 181-186. Springer Verlag, 
New York. 

, & W. A. Newman, 1975. A trilobitomorph 

origin for the Crustacea. Fossils and Strata 4: 437-459. 

Hou, X., 1987a. Two new arthropods from Lower Cambr- 
ian, Chengjiang, eastern Yunnan. Acta Palaeont. Sin- 
ica 26(3): 236-250, 2 figs, 4 pis. 

, 1987b. Three new large arthropods from Early 

Cambrian Chengjiang, eastern Yunnan. Acta Paleont. 
Sinica 26(3): 288, 4 pi.) 

, & J. Bergstrom, 1991. The arthropods of the 

Lower Cambrian Chengjiang fauna with relationships 
and evolutionary significance, pp. 179-187. in Simon- 
ette & Conway Morris (eds.). The early evolution of 
Metazoa and the significance of problematic taxa. 
Cambridge Univ. Press, London. 

, L. Ramskold, and J. Bergstrom, 1991. Composi- 
tion and preservation of the Chengjiang fauna, a Low- 
Cambrian soft-bodied biota. Zool. Scr. 20(4): 395. 

Johnson, R. G., & E. S. Richardson, 1969. Pennsylvanian 
invertebrates of the Mazon creek area, Illinois. The 
morphology and affinities of Tullimonstrum. Fieldi- 
ana. Geology 12(8): 119-149, figs. 63- 80. 

Kukalova-Peck, J., 1987. New Carboniferous Diplura, 
Monura, and Thysanura, the hexapod ground plan and 
the r61e of thoracic side lobes in the origin of wings 
(Insecta). Can. Jour. Zool. 65: 2327-2345. 

, 1992. The Uniramia do not exist: the 

groundplan of the Pterygota is revealed by Permian 
Diphanopterodea from Russia [Insecta: Palaeodicty- 
opteroidea]. Can. Jour. Zool. 79 (236). 


Lendzion, K., 1975. Fauna of the Mobergella zone in the 
Polish Lower Cambrian. Kwart. Geol. 19(2): 237-244 
4 figs. 

, 1977. Cassubia - a new generic name for 

Pomerania Lendzion, 1975. Kwart. Geol. 21(1): 211. 

Manton, S. M., 1972. The evolution of arthropodan loco- 
motory mechanisms. Part 10. Locomotory habits, mor- 
phology and evolution of the hexapod classes. Jour. 
Linn. Soc. (Zool,) 51: 203-400. 

, 1977. The Arthropoda. Clarendon Press. 

Oxford. 

Muller, K. L., 1983. Crustacea with preserved soft parts of 
the Upper Cambrian of Sweden. Lethaia 16: 93-109. 

, & D. Walossek, 1986. Martinssonia elongata, 

gen. et sp. n., a crustacean-like euarthropod from the 
Upper Cambrian "Orsten" of Sweden. Zool. Scr. 15 
(1): 73-92. 

Richardson, E. S., Jr., 1966. Worm-like fossil from the 
Pennsylvanian of Illinois. Science 151: 75-76. 

Ridley, M., 1990. Dreadful Beasts. London Review of 
Books. 28, June. 

, 1993. Analysis of the Burgess Shale. Paleo- 
biology 19(4); 519-521. 

Sanders, H. L., 1963. Significance of the Cephalocarida. In 
Phylogeny and Evolution of Crustacea. H. B. Whit- 
tington & W. D. I. Rolfe (eds.). pp. 163-175. Mus. 
Comp. Zool. Cambridge, Mass. 

Savory, T., 1964. Arachnida. Academic Press, New York. 
291pp., 102 figs. 

Schram, F. R., 1986. Crustacea. Oxford University Press, 
New York, 606 pp., Ulustr. 

, 1990. Review of Gould, S. J., 1989. Wonder- 
ful Life. Norton, N.Y. Jour. Crust. Biol. 10(3): 571-572. 

, & M. J. Emerson, 1991. Arthropod Pattern 

Theory : A new approach to arthropod phylogeny . Mem. 
Queensland Museum 31: 1-18, 12 figs. 

Sharov, A. G., 1966. Basic Arthropodan Stock. Pergamon 
Press, New York. 267 pp. 

Smith, E. L., 1990. An arthropod morphologist looks at six 
hundred million years of chelicerate evolution. Amer. 
Arachn. Soc., 14th Ann. Conf., Ottawa, 1990. Abstract. 

Snodgrass, R.E., 1956. Crustacean Metamorphosis. Smiths. 
Misc. Coll. 131(10): 78 pp., 28 figs. 

St0rmer,L., 1944. On the relationships and phylogeny of the 
fossil and Recent Arachnomorpha. Skr. Nor. Vidensk. 
Akad. Oslo I: Matemat. Naturvidensk. Klasse 5:1-58. 

, 1959. Trilobitoidea. In R. C. Moore (ed.). 

Treatise on Invertebrate Paleontology. Part O. Arthro- 
ropoda. I. pp. 23-37. 

Sturmer, W., & Bergstrom, J., 1976. The arthropods Mim- 
etaster ^n^Vachsonisia from Devonian shale. Palaeont. 
Zeitschr. 50(1/2): 1-112. 

Walcott, C. D., 1 9 12. Middle Cambrian Branchiopoda, Mal- 
acostiaca, Trilobita, and Merostomata. Cambrian Geol- 
ogy and Paleontology n. Smithsonian Misc. Coll. 57: 
145 - 228. 


AMPHIPACIFICA VOL. U. NO. 1 AUG. 31, 1995 34 


Walossek D., and K. L. Muller, 1989. A second type of A- 
nauplius from the Upper Cambrian ‘Orsten’ of Sweden 
Lethaia22: 302-306. 

Whittington, H.B., 1971. RQdQSchp\ion of Marrellasplend- 
ens (Tiilobitoidea) from the Burgess Shale, Middle 
Cambrian, British Columbia. Geol. Surv. Can. Bull. 
209: 1-24. 

, 1975. The enigmatic animal Opabinia 


regalis, Middle Cambrian, Burgess Shale, British Col- 

umbia. Phil. Trans. Roy. Soc. London B 271; 1-43. 

, & D. E. G. Briggs, 1985. The largest 

Cambrian animal, Anomalocaris, Burgess Shale, Brit- 
ish Columbia. Phil. Trans. Roy. Soc. B 309: 569-609. 

Wills, M. A., D. E. G. Briggs, & R. A. Fortey, 1994. Dispar- 
ity as an evolutionary index: a comparison of Cambrian 
and Recent arthropods. Paleobiology 20(2): 93-130. 



OpaBiniaTyttBs WaCcott 

MiddCe CamBrianJArtfiropod 


(SdananneCofBns UCustration, 
modified from Qotdd, 1S8S) 



AMPHIPACinCA VOL. 11 NO. 1, AUG. 31, 1995 35 

THE AMPHffOD SUPERFAMILY PONTOPOREIOIDEA ON THE PACIFIC COAST OF NORTH AMERICA. 
I. FAMILY HAUSTORHDAE. GENUS EOHAUSTORIUS J. L. BARNARD: SYSTEMATICS AND 

DISTRIBUTIONAL ECOLOGY 


ABSTRACT 


by E. L. Bousfield^ and Phillip Hoover^ 


On the Pacific coast of North America, from the Bering Sea to Southern California, the free-burrowing 
gammaridean amphipod family Haustoriidae is represented by six species of Eohaustorius Barnard, 1957. 
On the Asiatic Pacific coast six species, all subtidal, have now been described. A single northern subtidal 
species, E. eous, connects the two faunas in the Bering Sea region. 

This paper describes E. bamardi, new species, from off Pt. Conception, California, and provides re- 
descriptions, keys and new distributional information for Eohaustorius eous (Guijanova, 1951), E. estuarius 
Bosworth, 1973, £. sawyeri Bosworth, 1973, E. brevicuspis Bosworth, 1973, E. sencillus Barnard, 1962 and 
E. washingtonianus (Thorsteinson, 1941). Material ascribed to the latter species from the northwestern 
Pacific region by Gurjanova (1962) is herewith redescribed as E. gurjanovae, new species. Subtidal material 
from South Korea is described as E. longicarpus, new species. 

The species of Eohaustorius are morphologically variable throughout their ranges, especially E. 
washingtonianus, but variation is not considered of species or subspecies value. Cluster analysis reveals three 
main subgroupings, none very closely inter- or intra-related, viz: a North American endemic group of E. 
washingtonianus Barnard, E. brevicuspis Bosworth and E. bamardi, new species; an Asiatic Pacific group 
of E. cheliferus Bulcheva, E. subulicolus Hirayama and E. robustus Gurjanova; and a northern relatively 
primitive core group of E. eous (Guijanova), E. sawyeri Bosworth, E. gurjanovae, new species, E. estuarius 
Bosworth, E. longicarpus, new species, and E. sencillus Barnard. The Asiatic species have relatively 
restricted distributions and none is intertidal. This hiatus results presumably from competition with intertidal 
members of amphipod family Dogiehnotidae dominant in that region, and from severe physical factors in 
winter of low intertidal temperatures and ice scour. On the North American Pacific coast, however, all species 
have relatively wide geographical ranges, and four species are intertidal. There, only one species of 
Dogiehnotidae, Proboscinotus loquax, provides intertidal competition, and the climate is equable year-round 
winter ice scour is .lacking. 

The genus Eohaustorius is sufficiently similar to North American Atlantic haustorinid genera as to 
preclude separate evolution from a pontoporeiid ancestor and thereby render polyphyletic the family 
Haustoriidae. However, the genus Eohaustorius is cold-temperate, and the Atlantic-endemic genera are 
warm-temperate, in biogeographical affinities. Eohaustorius is closest morphologically to the Atlantic sub- 
tidal genus Pseudohaustorius, thereby raising the possibility that during early Miocene times, prior to emerg- 
ence of the isthmus of Panama, a common ancestor connected the two groups via a southern marine waterway. 


INTRODUCTION 

The superfaimly Pontoporeioidea is a relatively small 
group of fossorial amphipods, whose marine members are 
foundmainly in sedimentary substrata along holarctic shores. 
Members of the primitive family Pontoporeiidae tend to be 
arctic and sub-arctic in distribution, with a significant com- 
ponent confined to glacial relict freshwater lakes of North 
America and northwestern Eurasia (Bousfield, 1987). By 
contrast, members of the advanced and highly specialized 
family Haustoriidae are marine and estuarine and occur 
mainly along warm-temperate and boreal coastlines of the 
North Atlantic and North Pacific regions (Bousfield, 1965; 
1970, 1973). On the Pacific coast of North America, family 
Pontoporeiidae is sparsely represented (Bousfield, in prep: 
Priscillina and Monoporeia in the Bering Sea, Pontoporeia 
in glacial Qords, and Diporeia in a few post-glacial lake 
basins). However, owing mainly to the work of Thorsteinson 


T 


(1941), Gurjanova (1951, 1962), Barnard (1957, 1962), 
Bosworth (1973) and Coyle & Mueller (1981), the family 
Haustoriidae is known to be moderately speciose in shallow, 
high energy coastal marine waters from the Bering Sea coast 
of Alaska to southern California. The genus is well represented 
in coastal waters of Korea and Japan (Ishimarus, 1994), and 
along the Russian coast north to the Bering Sea region, but 
not in Arctic waters. 

Within the North Pacific region generally, the family 
Haustoriidae is represented only by the single genus, 
Eohaustorius Barnard, 1957. Some seven species of this 
genus have been recorded from the North American Pacific 
coast and another five from the Pacific coast of Russia and 
the Japan Sea (including Korea). The genus is distinct from 
the North Atlantic complex (with the European species 
Haustorius arenarius (Slabber) as type) in having peraeopods 
3 and 4 unlike in size and form, and telson lobes widely sep- 
arated on the dorsum of urosome 6, among other differences . 


Research Associate, Royal Ontario Museum, Toronto, Ontario. M5S 2C6. 

Research and Teaching Assistant, Department of Biology, University of Victoria, Victoria, B. C. V8W 2Y2. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 36 


This study treats the systematics and distributional ecol- 
ogy of species of the genus Eohaustorius in North Pacific 
coastal marine region, and emphasizes the North American 
Pacifica fauna. 

Species of Eohaustorius have proven useful as indicators 
of sediment quality (see Bousfield, 1991; Mcleay et al. 
(1990); Yeeetal. 1992). 

Acknowledgements. The present North American 
haustoriid material was accumulated mainly as a result of 
National Museum, now Canadian Museum of Nature (CMN), 
field expeditions, conducted by one of us (ELB) and 
colleagues, during the period 1955-1980. Complete lists of 
stations, pertinent data and acknowledgement of field 
assistance are provided elsewhere (Bousfield, 1958, 1963, 

1 968 ; Bousfield & McAllister, 1 962; and Bousfield & Jarrett, 
1981). Additional material was provided by Drs Peter 
Slattery, Moss Landing, California; Charles O' Clair, Auke 
Bay, Alaska; Kathleen Conlan CMN, Ottawa, and McLeay 
Associates, West Vancouver. The authors are most grateful 
for use of the laboratory facilites of Dr D. V. Ellis, University 
of Victoria, and for the use of collections and facilities of the 
CMN in Ottawa. 

The authors are indebted to Dr Weldon S. Bosworth for 
his pioneering work on much of this material in 1973-4, and 
for his unpublished commentary and distributional informa- 
tion. Susan Laurie-Bourque very capably assisted in 
preparation of the line drawings. Marjorie A. Bousfield 
provided translations of pertinent Russian literature. The 
illustrative work was supported under a research divisional 
grant of the Royal Ontario Museum, Toronto. 

SYSTEMATICS 

Haustoriidae Stebbing 

Haustoriidae Stebbing, 1906: 118. — Guijanova, 1951:328; 
1962: 395.— Bousfield, 1965: 165 (part); 1973: 99 (part); 
1982: 259. — Barnard and Drummond, 1982: 136. — 
Hirayama, 1985: 395. — Barnard & Karaman, 1991: 357. 

Taxonomic commentary. B amard and Karaman (1991) 
have provided a simplified key to genera of Haustoriidae 
(sensu strictu). 

With respect to superfamily classification, Barnard & 
Karaman (loc. cit.) have continued recognition of family 
Haustoriidae as the type of superfamily Haustorioidea, 
proposed initially by Barnard & Drummond (1982). As 
shown by Bousfield (1982b, 1990) and Bousfield & Shih 
(1994), the Bamardian concept (of Haustorioidea) includes 
most members of family Urothoidae and other superficially 
and convergently similar families. The latter groups are 
phyletically more correctly placed within superfamily 
Phoxocephaloidea (e.g., Bousfield 1982, 1990; and Schram, 
1 986). In all major character states, family Haustoriidae is 
most clearly related to members of family Pontoporeiidae, 


and thus phyletically assignable to the superfamily which the 

latter typifies, the Pontoporeioidea. As shown above 

(Bousfield, loc . cit.), these major pontoporeioidean character 
states of Haustoriidae, especially of its most primitive genus 
Protohaustorius, include its short broad, weakly rostrate 
head, "pseudorostrate" paired peduncles of antenna 1 , weakly 
(or non-) dactylate peraeopods and maxilliped, lack of coxal 
gill on peraeopod 7, unique form of the pleopods (lacking 
clothespin spines), strongly deflexed urosome, and the 
holarctic (non-antipodean) distribution of nearly all member 
species. The character states of the Pontoporeioidea, 
especially the phyletically significant antennal calceoli, are 
basically gammaroidean and not phoxocephaloidean or 
crangonyctoidean in form. 

Eohaustorius J. L. Barnard 

Eohaustorius J. L. Barnard, 1957: 81. — Gurjanova, 1962: 
400.— Bousfield, 1970: 150.— Bosworth, 1973: 160.— Barn- 
ard, 1975: 348 (key). — Hirayama, 1985: 43. — Barnard & 
Karaman, 1991: 361. — Ishimaru, 1994: 64. 

Type species. Haustorius washingtonianus Thorsteinson, 
1941, original designation. 

Component species. E. tandeensis Dang, 1968; E. 
subulicolus Hirayama, 1985; E. cheliferus (Bulycheva, 
1952); E. eous (Guijanova, 1951); £. robustus (Gurjanova, 
1953; E. sawyeri Bosworth, 1973; E. brevicuspis Bosworth, 
1973; E. estuarius Bosworth, 1973; E. longicarpus, new 
species; E. gurjanovae, new species; E. sencillus Barnard, 
1962; E. bamardi, new species. 

Diagnosis. Body short, broad. Head broad; rostrum 
short, acute. Pigmented eyes essentially lacking. Antennal, 
flagellum 5-segmented; accessory flagellum 2-segmented, 
attached subapically to peduncular segment 3, bearing 
aesthetascs. Antenna 2, peduncle 4 broadly lobate and 
strongly setose behind; peduncle 5 broad, not lobate behind; 
flagellum 4-5 segmented. 

Upper lip rounded. Lower lip, inner lobes with short 
proximal processes. Mandible, molar strong triturative; 
incisor acute; palp segment 3 with few (5-15) inner marginal 
comb spines. Maxilla 1 lacking accessory basal baler lobe; 
inner plate with single apical seta; outer plate with 8-9 apical 
spines. Maxilla 2, outer plate little larger than inner, not 
lunate inform; innerplate with weak facial setae. Maxilliped, 
inner plate with 2 apical spines; outer plate very large, 
exceeding palp segment 2; palp segment 3 clavate, not genic- 
ulate. 

Coxal plates 1 & 2 small, 3 & 4 squarish below. 
Gnathopod 1, segment 3 very short; segment 5 relatively 
short, deep; segment 6 medially deepest. Gnathopod 2, 
segment 3 very short; segment 5 with postero-distal cluster 
of specialized spines; segment 6 short, medially swollen, 
arcuate, produced beneath minute dactyl to form a microchela . 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 37 


KEY TO NORTH PACIFIC SPECIES OF EOHAUSTORIUS 


1. Pleon plate 3 strongly produced behind into a recurved hooklike process; peraeopod 4, hind lobe of 

segment 5 elongate, slender, length 4-5 X width (depth); uropod 3, inner ramus with single small inner 
marginal seta; Asiatic coast £. subulicolus (p. 42) 

— Pleon plate 3, hind process nearly straight, if hooked, not recurved; peraeopod 4, segment 5, hind lobe 
shorter, deeper, length less than 2 X depth; uropod 3, inner margin with 2-6 setae 2. 

2. Peraeopod 6, segment 4 tall, length 2X width, with 5-6 groups of facial spines (in addition to marginal 

spines); basis slender, distinctly narrower than length (depth), subovate; uropod 1, hind margin of inner 
ramus with 2 single setae; gnathopod 1, dactyl, body large, length > nail (unguis) 3. 

—Peraeopod 6, segment 4 subtriangular, widest distally, length < 2X width; basis as broader or broader 


than length; gnathopod 1, dactyl, nail longer than body 4 . 

3. Antennae 1 & 2, flagella 5-segmented; peraeopod 4, hind lobe elongate, ~2 X depth; abdominal side 

plate 3, apex abruptly upturned, minutely split-tipped E. longicarpus (p. 56) 

—Antenna 1 & 2, flagella 3-segmented; peraeopod 4, segment 5, hind lobe short, length not greater than 
depth; abdominal side plate 3, hind process straight or apex slightly upturned E. sencillus (p. 44) 


4. Peraeopod 4, segment 5, posterior lobe, distal margin with spine cluster; peraeopod 6, segment 4 with 

lower facial row of 2-3 spine groups; peraeopod 6, segment 5 with posterior marginal spine^roup . . 7. 
Peraeopod 4, segment 5, distal lobe base, smooth; peraeopod 6, segment 4 with at least one other spine 
cluster above lower row; peraeopod 6, segment 5 lacking posterior marginal spines 5. 

5. Peraeopod 7, basis, hind margin proximally with strong cusp or tooth; pleon plate 3 produced, poster- 
iorly as weak tooth £ washingtonianus (p. 50) 

Peraeopod 7, basis hind marginal tooth weak or rounded; pleon plate 3, process strong 6. 

6. Peraeopod 7, basis wider than deep, hind cusp rounded; maxilliped palp, segment 3 strongly broadened 

distally, width = 3/4 length e. brevicuspis (p. 50) 

Peraeopod 7, basis not wider than deep, hind cusp acute; maxilliped palp, segment 3 normal, length ~2X 

bamardi (p. 54) 

7. Peraeopod 4, segment 5, hind lobe strongly produced, width of segment 2 X depth (length); peraeopod 7, 
segment 6 with 2 posterior marginal groups of spines; gnathopod 2, basis, hind margin with distal setae only 

cheliferus (p. 55) 

— Peraeopod 4, segment 5, hind lobe normal, width about equal to length; peraeopod 7, segment 6 with 3-4 
posterior marginal spines groups; gnathopod 2, basis, hind margin setose throughout 8. 

8. Peraeopod 5, segment 4 widest distally, 2X length; pleon plate 3, postero-dorsal process large, strongly 

overhanging urosome; uropod 3, inner ramus with 2-3 marginal setae E. sawyeri (p. 44) 

Peraeopod 5, segment 4 less broad, ~ 1.5X length; pleon overhang normal, little or not exceeding side 
plate process; uropod 3, inner ramus with 5 marginal setae 9 

9. Peraeopod 7, segment 6 with 2 groups of posterior marginal spine groups; coxae 3 & 4 antero-distal mar- 
gins rounded Eestuarius (p. 40) 

Peraeopod 7, segment 6 with 3-4 posterior marginal spine groups; coxae 3 & 4 squarish 10. 

10. Peraeopod 5, segment 6 with 1 group of anterior marginal spines; pleon plate 3 , hind process, apex 

slightly upturned; peraeopod 4, segments 5 & 6 lacking anterior marginal spines; peraeopod 7, basis 
veiy broad, exceeding length £ (p 43 ^ 

—Peraeopod 5, segment 6 with 2 groups anterior marginal spines; pleon plate 3 hind process straight; per- 
aeopod 4, segment 5 & 6 with anterior marginal spines; peraeopod 7, basis not wider than deep . . .\ 1 1. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 38 

11. Peraeopod 7, segment 6 with 4 posterior marginal spines; basis lacking posterior cusp; mandibular palp 

segment 3 with 14-15 posterior marginal comb spines E. eous (p. 38) 

— Peraeopod 7, segment 6 with 3 posterior marginal spines; basis with rounded posterior proximal cusp; 
mandibular palp segment 3 with 8-9 posterior marginal comb spines E. gurjanovae (p. 47) 


Peraeopod 3, segment 4 short, triangular; 5 weakly lob- 
ate behind; 6 small, margins spinose, not setose. Peraeopod 
4 smaller and unlike peraeopod 3 in form; segment 3 very 
short, 4 little broadened, 5 strongly produced and spinose 
behind; 6 slender, distally spinose and setose. 

Peraeopod 5, basis broad, hind margin setose, with 
proximal cusp; segments 4-6 not broader than long, outer 
face with spine clusters . Peraeopod 6 longest; basis medium 
broad, hind margin setose, with proximal cusp; segment 4 
often longer than broad; segment 5 broader than long, with 
prominent antero-distal process and distal marginal notch; 
segment 6, some distal spines split-tipped. Peraeopod 7, 
basis very broad hind margin nearly bare, proximal cusp low 
or lacking; segment 4 broad, triangular; segment 5 broad. 

Pleon segment 3 strongly deflexed posteriorly, postero- 
distal lobe strong, overhanging urosome. Pleon plate 3, hind 
comer acutely produced. Pleopods powerful; peduncle 
short, broad; outer ramus 10-16 segmented, inner shorter, 
with proximal baso-medial lobe. 

Urosome short, lacking antero-distal lappet. Uropod 1, 
rami cylindrical, inner ramus with posterior marginal setae 
only. Urosome 2 short, not occluded dorsally. Uropod 2, 
rami heavily setose, subequal. Uropod 3, rami short, <2X 
peduncle, terminal segment variable. Telson lobes widely 
separated at base; each with dorso-lateral marginal setae, and 
single apical penicillate seta. 

Coxal gills saclike, on peraeopods 2-6. Brood plates 
relatively narrow, elongate. 

Distribution. Member species are endemic to the North 
Pacific coastal shelf regions of eastern Asia, and North 
America, from the Bering Sea to Vietnam in the west, and in 
the east, south to Baja California. 

Taxonomic commentary. Eohaustorius is distinct 
from North American Atlantic genera in the unlike form of 
peraeopods 3 & 4 and the widely separated telson lobes. 
However, in the short antennal flagella, form of the lower lip, 
maxilla 1 & 2, maxilliped, processiferous pleon plate 3, and 
setose telson, it more closely resembles the warm-temperate 
North Atlantic genus Pseudohaustorius (Fig. 2, p. 41) than 
the type genus Haustorius (Fig. 2.2). Such basic similarities 
suggest a former ancestral link with the diverse Atlantic 
haustoriid complex via the submerged Panama isthmus 
(Bousfield, 1970) (see also pp. 61-62). 

Eohaustorius eous (Gurjanova) 

<Figs. 1, 2) 

Haustorius eous Gurjanova, 1951: 331. 

Eohaustorius eous eous Gurjanova, 1962: 406. 
Eohaustorius eous Barnard & Karaman, 1991: 463. — Ishi- 
maru, 1994: 64. 


LEGEND FOR FIGURES 


A1 

antenna 1 

MX 1 - 

maxilla 1 

A2 

antenna 2 

MX2 - 

maxilla 2 

BR. 

coxal gill 

MXPD - 

maxilliped 

BR SET - 

brood plate seta 

O.P. - 

outer plate 

COXAE - 

coxal plates 

PLP - 

palp 

DACT - 

dactyl 

P3-P7 - 

peraeop'ds 3-7 

EPl-3 - 

pleon plates 1-3 

RT 

right 

GNl 

gnatho;od 1 

SP 

spine 

GN2 - 

gnathopod 2 

T 

telson 

I.P. 

inner plate 

U1-U3 - 

uropods 1-3 

I.R. 

inner ramus 

UROS - 

urosome 

LFT 

left 

X 

magnified 

LL 

lower lip 

o 

male 

MD 

mandible 

0 

female 


Material examined. 

ALASJCA. Bering Sea: Northeast end of St. Lawrence I., Lot 
#1, 20 m sand, P. Slattery coll., July 10, 1980 - 2 males, 4 
females, 1 im, CMN Cat. no. NMCC 1991-1209; Ihid.. Lot #5 

- 2 males, 13 female, 5 im. 

St. Mathew I., Walrus Cove, sand, 8 m,P. Slattery coll., 1983 
- 1 im; Ibid .. 11m scoop, sand - 3 males, 1 1 females, 2 im; 
Ibid .. 13 m, sand - 2 males, 21 females, 14 im. CMN Cat. no. 
NMCC1991-1206. 

St. Paul L, English Bay, 3 m scoop, P. Slattery coll., 1983, 

- 5 males, 37 females, 8 im; Ibid .. 10 m sand - 3 males, 9 
females, 2 im; Ibid ., reef, 20 m - 1 female ov (5.5 mm) slide 
mount, 3 females (5.5 mm, 5.5 mm, 4.5 mm)+ 1 male, 4 
females, 15 im, NCMNB Cat. no. NMCC1991-1204; Ibid .. 
25 m sand - 3 males, 36 females, 15 im, CMN Cat. no. 
NMCC1991-1203. 

Alaska mainland: 30 miles west Cape Rodney, 24 m. dive, P. 
Slattery coll., 1981 - 6 females, 3 im, CMN Cat. no. NMCC- 
1991-1211. 

Diagnosis. Female (6.0 mm): Head, rostrum short. 
Pigmented eyes lacking. Antenna 1, segment 2 strongly 
setose anteriorly; accessory flagellum inserted nearly apic- 
ally. Antenna 2, peduncular segment 4, postero-distal lobe 
medium; posterior margin lined with numerous (>40) plumose 
setae; segment 5 medium broad, widest distally; flagellar 
segment 1 with postero-distal setal cluster. 

Mandible, palp segment 3 with 14-15 posterior mar- 
ginal comb spines. Maxilla 2, inner plate with distinct facial 
row of 6-7 plumose setae. Maxilliped, outer plate medium; 
palp segment 2, inner lobe large, broad, reaching almost to 
tip of narrowly clavate segment 3. 

Coxae 1 & 2. Gnathopod 1 , segment 5 relatively short, 
deep; segment 6 medium, arcuate. Gnathopod 2, hind margin 
long-setose; segment 5 slender, shallow, distal spines slender. 

Peraeopod 3, coxa squarish; segment 4 short, distally 
broad; segment 5 strongly setose proximally; segment 6 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 39 



FIG. 1. Eohaustorius eous. (Gurjanova). Female ov. (5.0 mm). Bering Sea, Alaska. Slattery coU. 


ovate, margins spinose. Peraeopod 4, segment 4 with 23 

posterior marginal setae; segment 4 hind lobe short, distally 
broad, truncate, anterior margin with 1 stout spine group; 
segment 6 slender, with 21 anterior marginal spine group. 

Peraeopod 5, basis broadly ovate, hind margin com- 
pletely lined with setae; segment 4 short, uniformly broad; 
facial spine clusters strong; segment 5 medium, not wider 
than long, facial spine clusters strong; segment 6 broadest 
medially, anterior margin with 2 spine clusters, posterior 
margin with 2 single spines. Peraeopod 6, basis medium, 

hind margin setose throughout; segment 4 elongate, with 3- 

4 facial spine clusters; segment 5 broadest distally, with 2 


weak facial spine groups, 4-5 inner distal and 5-6 outer distal 

marginal spines; antero-distal emargination medium deep; 
segment 6 relatively long and slender, with 4-5 clusters of 
mixed long and short spines. Peraeopod 7, basis broad, hind 
margin distally narrowing and lined with medium setae; 
segment 4 slightly wider than long, anterior margin with 3 
spine clusters, posterior margin lined with long setae; seg- 
ment 5 squarish, anterior margin with 1 cluster of long 
spines; segment 6 little broadened, anterior margin with 1, 
and posterior margin with 4, clusters of medium spines. 

Pleopods, basis stout, broad, outer margin strongly 
plumose-setose; outer ramus 15-segmented, inner 12-seg- 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 


40 



FIG. 2 Eohaustorius eous (Gurjanova) Female ov. (6.0 mm). East coast Kamchatka peninsula. 

(after Gurjanova, 1962) 


merited. Pleon plate 3, hind comer strongly produced, nearly 
straight, acute. Uropod 1, peduncle, outer margin with 4- 
5 slender spines; inner ramus, posterior margin with short 
spines. Uropod 3, outer ramus, terminal segment short (<1/ 
2 proximal segment); inner ramus, inner margin with 3 
plumose setae. 

Telson lobes short, slender, with 12 dorso-distal setae. 


from the northern Sea of Okhtosk, illustrated in Guijanova 
(loc. cit., fig. 1 36B2) is here considered a variant on the main 
theme from the Kamchatka pensinsula andBering Searegions. 

Eohaustorius estuarius Bos worth 
(Figs. 4) 


Distribution. Eastern Kamchatka & Bering Sea, 20-40 
m; western Bering Sea, subtidally to 25 m. Not taken in 
southeastern Alaska despite apparently suitable habitat (e.g. , 
Glacier Bay) where E. washingtonianus was dominant. 


Eohaustorius estuarius Bosworth, 1973: 253, fig. 2 im. — 
Staude, 1987: 372 (key), 383 , fig. 18.11 .—Barnard & Kara- 
man, 1991: 363. 

Material examined. 10 lots containing 158 specimens: 


BRITISH COLUMBIA. 


Taxonomic commentary. E. eous is a relatively primi- 
tive species, showing several plesiomorphic character states 
in common with the N. America estarine species E. estuarius. 
It is not closely related to E. robustus, differing in the 
character states noted in the key and on p. 37. The material 


Queen Charlotte Islands, ELB Stns., July-Aug., 1957 (~10 
specimens at 3 stations, verified by W. Bosworth, 1973): 
H8a (Delkatla Slough) - 3 females; HIO (New Masset) - 1 
female; W 1 (north end Lepas Bay) - 8 males 1 2 females, 6 im. 
Vancouver I., northend, ELB Stns., 1959: 012, AhousBay, 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 41 



FIG. 3. Pseudohaustorius caroliniensis Bousfield. Female (7.6 mm), lateral view; mouthparts, telson 
2. Haustorius canadensis Bousfield. Female (12.0 mm), mouthparts, telson. (after Bousfield, 1973). 


Vargas I. - 3 males, 1 fern, 1 im; Stn. 013, Yarksis, Vargas 
I. - 4 males, 5 females, 1 im. 

Central Vancouver I., ELB Stns.,1955: PI, Clayoquot I. - 1 
female, 1 im; P6a, southeast end Wickaninnish Bay - 1 1 
males, 26 females. ELB Stns., July, 1970: P701, south end 
Long Beach, in surf-exposed sand at freshwater beach seep, 
LW level - 1 female ov. (5.0 mm), (slide mount) (fig’d 
specimen), + 17 males, 33 females, CMN Cat. no. 
NMCC 199 1-1229; P708, Pachena Bay, mouth of estuary - 
numerous specimens. 

WASHINGTON. OREGON. 

ELB Stn. W34, Crescent Beach, east end, near creek mouth- 
1 female (4.8 mm), slide mount, -i-12 other females, 5 males, 
CMN Cat. no. NMCC- 1992- 1255; Stn. W41. Sooes estuary, 
near mouth, in steep sand banks - 1 im. 

Diagnosis. Female (5.0 mm): Head, rostrum medium; 
eyes small, weakly pigmented. Antenna 1, peduncle 2, 
anterior margin setose nearly to base. Antenna 2, peduncular 
segment 4, postero-distal lobe large, posterior margin with 
25+ plumose setae; segment 5 distally broadest; flagellar 
segment 1 with distal plumose seta. 

Mandible, palp segment 3 , inner (posterior) margin with 


10-12 marginal comb spines, outer margin with 5-6 mediums 
etae. Maxilla 2, inner plate with strong facial row of setae. 
Maxilliped, inner plate tall, slender; outer plate broad, distally 
truncate; palp segment 2, inner lobe long narrow, reaching 
tip of broadly expanded palp segment 3. 

Gnathopod 1, basis, anterior margin weakly setose 
throughout; carpus short, deep; dactyl, nail long. Gnathopod 
2, carpus relatively short and deep, with sub-apical postero- 
distal cluster of slender spines. 

Peraeopod 3, coxae expanded anteriorly, basis with 
antero-distal cluster of setae. Peraeopod 4, segment 4 with 
2 posterior marginal plumose setae; segment 5, hind lobe 
medium, proximal margin with a few setae, anterior margin 
with strong oblique spine row, hind margin truncate, spinose; 
segment 6 medium, little broadened distally, with single 
oblique anterior marginal spine group. 

Peraeopod 5, coxal hind margin strongly setose; basis 
medium, hind margin proximally setose; segment 4 rela- 
tively short, broad, facial spine groups strong; segment 5 
shorter than broad, facial spines strong; segment 6 broadest 
medially, with2 anterior marginal spine groups, hind margin 
with single spine cluster. Peraeopod 6, basis medium, hind 
margin distally bare; segment 4 relatively short, broadest 
distally, with 4 weak facial groups of spines; segment 5 




AMPHIPACMCA VOL. 11 NO. 1, AUG. 31, 1995 42 



FIG, 4, Eohaustorius estuarius Bosworth, Female ov (5.0 mm) Long Beach, V. L, B. C. 

(partly after Bosworth, 1973) 


broader than deep, with 2 small facial clusters of spines, 3- 
4 spines along inner distal margin, and 9-10 spines along 
outer distal margin; segment 6 with 6-7 posterior marginal 
clusters of short and long spines. Peraeopod 7, basis broadly 
expanded, lacking proximal basal cusp, hind margin nearly 
bare; segment 4 short, very broad distally, anterior margin 
with 2 spine clusters, posterior margin lined with plumose 
setae throughout; segment 5 short, broader than deep, with 2 
anterior marginal spine clusters; segment 6 broad, anterior 
margin strongly convex with single cluster of strong spines, 
posterior margin with 2 spine clusters. 

Pleopods normal for the genus. Pleon plate 3, hind 
comer strongly produced, straight, acute. Uropod 3 rami 
relatively short, <2X peduncle; outer ramus medium; inner 
ramus with few inner marginal seta. 

Telson lobes medium broad, regularly setose. 

Distribution. Common in freshwater intertidal seeps 
and rills over open and/or protected sand beaches, from 
Central California north through Oregon, Washington, and 
British Columbia to Dixon Entrance; not yet taken in south- 
eastern Alaska. 


Taxonomic commentary. As noted elsewhere (p. 59), 

this specis shows mainly plesiomorphic character states. It 
is a member of the E. eous subgroup and similar to E. 
gurjanovae of the Asiatic North Pacific region.. 

Eohaustorius subuUcolus Hirayama 
(Fig. 5) 

Eohaustorius subulicolaRiTSiy ama, 1985: 43, figs. 155-157. 
Eohaustorius subulicolusBamaid&Karaman, 1991: 463. — 
Ishimaru,1994: 64. 

Diagnosis. Male (2.25 mm): Head, rostmm short, de- 
curved. Pigmented eyes lacking. Antenna 1, accessory flag- 
ellum medially inserted on peduncular segment 3. Antenna 
2, peduncular segment 4, antero-distal lobe shallow; hind 
margin with few (~17) plumose setae; segment 5 of medium 
width; flagellar segment 1 with single large postero-distal 
seta. 

Mandibular palp, segment 3 with few (4-5) comb spines. 
Maxilla 1, outer plate with 8 apical spines. Maxilla 2, inner 
plate with 6-7 submarginal facial row of setae. Maxilliped, 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 43 



FIG. 5. Eohaustorius subulicolus Hirayama. Male 

palp segment 3 narrowly clavate; outer plate narrow. 

Coxa 1 vestigial; coxa 2 small rounded below, hind mar- 
gin with single seta. Gnathopod 1 , segment 5 short and deep; 
segment 5 slender. Gnathopod 2, basis with ~5 hind mar- 
ginal setae; segment 5 with 5 distally spoon-shaped spines. 

Peraeopod 3, basis, hind margin with distal setae only; 
segment 5, hind margin lacking proximal setae; segment 6 
narrow. Peraeopod 4, coxa slender smoothly convex in 
front; basis hind margin bare; segment 4 with 4 posterior 
marginal setae; segment 5 (carpus), posterior lobe slender 
acute, lacking spines; segment 6 slender, with apical spine(s) 
only. 

Peraeopod 5, basis, posterior margin setose throughout; 
segment 4 narrow, longer than broad, facial spines medium; 
segment 5 slender; segment 6 slender, with single anterior 
marginal spine. Peraeopod 6, basis, hind margin setose 
throughout; segment 4 little broadened, facial spines lack- 
ing; segment 5 broadest distally, lacking facial spines, distal 
margin with a few spines near hinge; segment 6, postero- 
distally with slender split-tipped spines and long setae. Per- 
aeopod 7, basis lacking proximal cusp, hind margin straight. 


(2.25 mm). Tomioka Bay. (after Hirayama, 1985). 

nearly bare; segment 4 slender, hind margin nearly bare; 
segment 5 as long as broad, anterior margin with 3-4 slender 
spine groups; segment 6 slender with single anterior mar- 
ginal spine cluster and elongate pectinate apical spines. 

Pleopods, peduncle small; rami slender, outer ramus 9- 
10-segmented. Pleon plate 3, hind corner strongly produced, 
hooklike, extending well beyond postero-dorsal process. 
Uropod 1, rami with apical spines and setae. Uropod 3, rami 
slender; inner ramus lacking inner marginal setae; outer 
ramus, terminal segment strong (> 2/3 inner segment). 

Telson lobes slender, marginal setae few. 

Distribution. Tomioka Bay, Japan; subtidal. 

Taxonomic commentary. Eohaustorius subulicolus is 
distinctive on the basis of reduction of some character states, 
and special development of others. Hirayama (1985) des- 
cribed the species from the type male and four additional 
specimens. He noted its general resemblance to F. cheliferus. 
but E. subulicolus may qualify for separate subgeneric 
status. 



AMPHIPACMCA VOL. 11 NO. 1, AUG. 31, 1995 44 


Eohaustorius sawyeri, Bos worth 

(Fig. 6) 

Eohaustorius sawyeri Bosworth, 1973: 257, fig. la-e. — 
Austin, 1985: 607. — Staude, 1987: 383, 372 (key). — Barnard 
& Karaman, 1991: 363. 

Material examined. Six lots containing 37 specimens 
(both sexes and subadults), from 4 localities in British Col- 
umbia, and two in California: 

BRITISH COLUMBIA. 

Vancouver I., southern end: Off Long Beach, V. I., 22 m, P. 
Slattery Stn., 1982 - 3 males, CMN Cat. no. NMCC1991- 
1219. ELB Stn. P21a, Trevor Channel, off Bordelais I., 44 
m, fine sand, Aug. 9, 1975 - 1 female (3.2 mm) (slide mount) 
(figured specimen) , CMN Cat. no . NMCC 1991-1227; Ibid . , 
Stn. B9c, off Second beach, 20-25 m, medium sand, June 28, 
1976 - 1 female; ELB Stn. H41, Jordan R., black silty sand, 
LW, July 27, 1964 - female ov (5.2 mm). 

CALIFORNIA 

Off Marine Laboratory, Moss Landing, 2 m sand, P. Slattery 
coll., June 1, 1982 - 2 males, 7 females, CMN Cat. no. 
NMCC1991-i240; Ibiil. 12 m, July 1, 1982 - 5 males, 8 
females, CMN Cat. no. NMC1991-1239. 

Diagnosis. Female im. (3.2 mm.): Head, rostrum. Eyes 
whitish, not pigmented. Antenna 1, peduncle 2, anterior 
margin weakly setose, singly inserted. Antenna 2, peduncle 
4, postero-distal lobe medium, posterior margin with 30+ 
plumose setae, antero-distal lobe strong, extending >2/3 
length of segment 5; segment 5 relatively shallow; basal 
flagellar segment with 3-4 distal plumose seta. 

Mandible, palp segment 3 with 8-11 posterior marginal 
comb spines. Maxilla 1, palp stout, proximal segment short 
(< 1/2 segment 2). Maxilla 2, inner plate, facial setae submar- 
ginal. Maxilliped, outer plate medium; palp segment 2, inner 
lobe narrow, shorter than medium-large segment 3. 

Gnathopod 1, coxa subquadrate; basis broadened medi- 
ally, anterior margin smooth distally; segment 5 elongate, 
medium deep; segment 6, thick (deep). Gnathopod 2, basis, 
anterior margin smooth; segment 5 slender, lower margin 
straight. 

Peraeopod 3, coxa 3 subquadrate; segment 4 short, very 
broad distally; segment 5 deep, with antero-proximal in- 
vagination, hind margin proximally setose; segment 6 large, 
lozenge-shaped, margins slender- spinose. Peraeopod 4, seg- 
ment 4 with 4 postero-marginal setae; anterior margin with 
distal spine group; segment 5, anterior margin with fan- wise 
spine row, hind lobe short, postero-proximal margin with 2 
spine clusters; segment 6 stout, broadening distally, with 2 
anterior and 2 posterior marginal spine clusters. 

Peraeopod 5, basis broadly ovate, hind margin nearly 
bare distally; segment 4 short, strongly broadest distally, 
facial spines strong; segment 5 expanding distally, longer 
than broad, facial spines strong; segment 6 broad, apex 
truncate, anterior margin with 1, posterior margin with 3 


spine clusters. Peraeopod 6, basis medium broad, hind 

margin lightly setose proximally; segment 4 long, broadest 

distally, with several strong facial spine clusters; segment 5 
broadening distally, with 2 strong facial spine clusters antero- 
distal margin with 12-15 spines, excavation shallow; seg- 
ment 6 slender, with 4-5 posterior marginal spine clusters. 
Peraeopod 7, posterior margin of coxa broadly acute; basis 
broad, convex hind margin distally with a few short setae, 
lacking proximal cusp; segment 4 short, broadest distally, 
hind margin setose; segment 5 broader than deep, anterior 
margin with single spine group, antero-distal free margin 
broad, lined with spines, postero-distal angle with long 
heavy spine; segment 6 broad, anterior margin with 1, post- 
erior margin with 3-4 stout spine groups. 

Pleopods, peduncle short broad, outer margin strongly 
plumose- setose; outer ramus 16-segmented, inner ramus 13- 
segmented. Pleon plate 3, hind corner moderately produced, 
acute, strongly overhung by, and much shorter than, postero- 
dorsal process of pleosome 3. Uropod 1, peduncle, outer 
margin with 3-4 slender spines, distal spine cluster medium; 
inner ramus posteriorly setose; outer ramus narrow, apex 
sub-acute. Uropod 3, outer ramus slightly the longer, terminal 
segment medium; inner ramus lacking inner marginal setae. 
Telson lobes short, broad, with few dorso-distal setae. 

Distribution. A southern species, abundant along coasts 
of California and Oregon, diminishing in Washington, and 
barely entering British Columbia. Occurs along outer surf- 
exposed sand beaches, from MLW to shallow subtidally. 

Taxonomic Commentary. The large female specimen 
from Jordan R. exhibited a very broad segment 6, and heavy 
facial spines on segments 4 & 5 of peraeopods 5 and 6. 

Eohaustorius sencillus J. L. Barnard 
(Fig. 7) 

Eohaustorius sencillus Barnard, 1962: 249, figs 1, 2. — Bos- 
worth, 1973: 8 (key). — Barnard, 1975, fig. 44. — Barnard & 
Karaman, 1891: 363. 

Material examined. Mile buoy, off Moss Landing, 
California, 20 m sand, P. Slattery coll., Feb. 24, 1971 - 1 
female (slide mount) (figured specimen), CMN Cat. no. 
NMCC1991-1241; 13 additional females, 2 males. 

Diagnosis. Female (3.5 mm): Head, rostrum short. 
Pigmented eyes lacking. Antenna 1 , peduncular segment 2, 
anterior margin weakly setose, bare proximally. Antenna 2, 
peduncular segment 4 relatively short and deep, postero- 
distal lobe medium, hind margin with 25-30 plumose setae; 
segment 5 as deep as long; basal flagellar segment postero- 
distally with 4-5 long setae. 

Mandible, palp segment 3 slender, with 7 posterior 
marginal comb spines. Maxillae undescribed. Maxilliped, 
outer plate broad; palp segment 2, medial lobe large, broad, 
shorter than moderately broadened terminal segment. 


. AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 45 



FIG, 6. Eohaustortus sawyeri Bosworth, 1973. Female ov ( 3.2 mm ). Off Long Beach, V.I., B.C. 

Coxae 1 & 2 squarish below. Gnathopod 1 , basis with 

7-8 posterior marginal setae; segment 5 medium, deep, 
convex below; segment 6 sharply broadest medially; dactyl, 
unguis large, heavy. Gnathopod 2, basis lined posteriorly 
with longish setae; segment 5 slender, strongly setose; 
postero-distal spines few, weak; segment 6 slender, regular. 

Peraeopod 3, coxa deep, sublunate; segment 4 medium 
broad distally, hind margin with 7-9 setae; segment 5 rela- 
tively shallow, anterior margin bare, not emarginate proxi- 
mally, lower margin proximally setose; segment 6 lenticular. 


margins slender spinose. Peraeopod 4, segment 4 relatively 
large, hind margin convex, with 2-3 long setae, anterior 
margin with weak oblique spine row; segment 5, with weak 
anterior oblique spine row, posterior lobe medium, rounded 
behind, with 2 weak postero-proximal spine groups; seg- 
ment 6 slender, with anterior marginal spine cluster, and 2 
postero-distal single marginal spines. 

Peraeopod 5, basis ovate, hind margin lacking distal 
setae; segment 4 not broader than deep, parallel-sided, facial 
spine groups weak; segment 4 relatively small, not wider 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 46 



FIG 7. Eohaustonus sen ciUus Barnard, 1962. Female (3.5 mm). Off Moss La nding, California. 

than deep facial spine groups weak; segm ent 6 not br^- Pleon plate 3. hind comer acutely produced, short Up 

ened, anterior and posterior margins each with 2 single directly beneath dorsal we^ Tne; 

snines anex narrowly truncate, weakly spinose. outer margin nearly bare, distal spine cluster weak, inner 

Peraeopodb coxa narrow, deep; basis relatively little broad- ramuswealdysetosepostenorly;outerramus,postenormM- 

Ined h^d margin with proxLal setae only; segment 4 gin with slender spines. Uropod 3 rami ^ 

donaate broadest medially, with 6 small facial spine clus- -2X peduncle; outerramus,ternmn^ segment very short (<U 

2rs segment 5 not broadL than deep, with single facial 3 proximal segment); innerrarnus, ^nd margin 

Se anXdistalmarginwith4-5spines,excavationdeep; Telson lobes short, broad, with 6-8 dorso-distal setae. 

4 longer than broad, gently broadening distally, anterior not reaching Canadian waters. 


margin with 2 spine clusters, hind margin with 5 plumose 
setae; segment 6 slightly broader than deep, with anterior 
spine cluster; anterior distal free margin relatively short; 
segment 6 medium broad, anterior margin with 1 , posterior 
margin with 3-4 spine clusters, apex truncate, spinose. 


Taxonomic Commentary. This species is distinguished 
by the relatively large basis of peraeopod 7, and large dactyl 
of gnathopod 1. Bosworth (pers. communic.) recognized a 
variant in deeper water material of J. L. Barnard (loc. cit.). 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 


47 



FIG. 8. Eohaustorius gurjanovae, new species. Female ov (6.Q mm). Southern Sakhalin I., Sea of Japan. 
(modified from Gurjanova, 1962) 


Eohaustorius gurjanovae^ new species 

(Fig. 8) 

Eohaustorius washingtonianus Gurjanova, 1962: 404, figs 
135B, V. 

Type material. Female ov (6.0 mm), Holotype; 7 
females and males, Paratypes, from south coast of Sakhalin 
I., Sea of Japan; collections of the Zoological Museum, St. 
Petersburg, Russia. 

Diagnosis. Female (7.0mm): Head, rostrum short; pig- 
mented eyes lacking. Antenna 1 , peduncle 2 anteriorly setose 
throughout. Antenna 2, peduncular segment 4, posterior 
margin with 25-30 plumose setae; postero-distal lobe large, 
extending to mid-point of deep segment 5; basal flagellar 
segment with 1 stout postero-distal plumose seta. 

Mandibular palp medium, with 7-8 posterior marginal 


comb-spines. Maxillae 1 & 2 undescribed. Maxilliped, outer 
plate slender, tall; palp segment 2, inner lobe slender, long, 
nearly reaching tip of clavate palp segment 3. 

Gnathopod 1, coxa, hind comer squarish; dactyl, body 
palm-shaped, unguis large. Gnathopod 2, basis, posterior 
margin lined with medium setae; segment 5 slender, postero- 
distal spine cluster strong; segment 6 much shorter, slender. 

Peraeopod 3, coxa, anterior margin rounded; basis thick, 
heavy; segment 4 short, expanding to broad distal margin, 
antero-distal angle and posterior margin with several plumose 
setae. Peraeopod 4, coxa subquadrate, lower and hind marg- 
ins setose; basis with a few postero-distal setae; segment 4, 
hind margin with 3-4 plumose setae, anterior margin with 
medial cluster of slender spines; segment 5 hind lobe short, 
anterior margin with oblique row of stout spines, postero- 
proximal margin with 2 groups of stout spines; segment 6 
short, broadening distally to large apical cluster of spines, 
anterior margin with single spine cluster and a few setae. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 48 


Peraeopod 5, basis broad, orbicular, hind margin devoid 
of setae except proximally and mid-distally; segment 4 
broadening gradually, longer than wide, with clusters of 
stout facial spines; segment 5 smaller and narrower, facial 
spines strong; segment 6 broad, anterior margin with 2 
clusters of stout spines, posterior margin with 2 singly 
inserted spines, apical spines strong. Peraeopod 6, basis 
medium broad, hind margin setose throughout, except for 
short distal gap; segment 4 short, very broad, with 2 anterior 
clusters and 1 posterior submarginal row of stout spines; 
segment 5 much broader than deep, with 2 facial spine 
clusters, and 6-7 antero-distal marginal spines, distal exca- 
vation medium deep; segment 6 large, bent forward, hind 
margin with 6 clusters of spines, some elongate distally. 
Peraeopod 7, basis very broad, hind margin with 4-5 medio- 
distal setae and blunt proximal cusp; segment 4 broadly 
triangular, anterior margin with 2 spine clusters, hind margin 
setose throughout; segment 5 large, slightly broader than 
segment 4, anterior margin with 2 spine clusters, antero- 
distal free margin heavily spinose, postero-distally angle 
with medium stout spine; segment 6 medium, anterior mar- 
gin with 3-4, and posterior margin with 3, spine clusters, 
some spines elongate, apex broad, heavily spinose. Long 
anterior marginal spines are split-tipped or clavate. 

Pleon plate 3, hind comer normally produced, acute, not 
elongate, with several lower marginal and submarginal 
plumose setae. Uropod 1, peduncle, outer margin weakly or 
not spinose; outer ramus, posterior margin with subapical 
fan of spines; inner ramus, posterior margin distally with 
long setae. Uropod 2, peduncle and rami regularly setose. 
Uropod 3, rami subequal, shorter than 2X peduncle; terminal 
segment of outer ramus short; inner ramus with 4-5 inner 
marginal setae. Telson lobes slender, each with 5-6 dorso- 
distal plumose setae and several inner marginal fine setae. 

Etymology. The species is named in honour of the late 
Eupraxie F. Guijanova who first recorded and figured the 
material from the Soviet far eastern region, as reproduced 
here. 

Distribution. South coast of southern Sakhalin I., Sea 
of Japan, in sand at 19 m. depth. 

Taxonomic commentary. E. guijanovae is another 
member of the advanced group of species including E. rob- 
ustus, E. cheliferus and E. washingtonianus. As noted by Dr 
Gurjanova (loc. cit., p. 405), this species differs from the 
North American Pacific species, E. washingtonianus, in a 
number of morphological character states, including the 
stronger armature of peraeopods 5-7, the more numerous 
carpal spines of gnathopod 2, and the linear setose lobes of 
the telson. Together these two forms do not qualify as a pan- 
Pacific sibling species pair and are here considered distinctly 
separate species. 


Eohaustorius robustus (Gurjanova) new status 

(Fig. 9) 

Haustorius eous robustus Guijanova, 1953:216. 
Eohaustorius robustus eous Guijanova, 1962:409. — Barnard 
& Karaman: 363. 

Material examined. No specimens were taken in the 
North American study region. 

Diagnosis. Female (6.5 mm): Head, rostrum short. Pig- 
mented eyes lacking. Antenna 1 , flagellum short, peduncular 
segment 2 with thick, coarse, facial plumose seta distally. 
Antenna 2, peduncular segment 4 short and deep, hind 
margin with -35 plumose setae; postero-distal lobe large; 
segment 5 deepest mid-distally; basal flagellar segment 
postero-distally with 3 short plumose setae. 

Mandibular palp, segment 3 relatively broad, shorter 
than 2 relatively, with 7 posterior marginal comb spines. 
Maxillae and maxillipeds not described or figured. 

Coxae 1 & 2 small, regular. Gnathopod 1 , basis, hind 
margin sparsely setose; segment 5 large, deep, strongly 
setose behind; segment 6 short broad; dactyl with long 
straight unguis. Gnathopod 2, basis, hind margin with 
several long setae; segment 5 elongate, postero-distal spines 
numerous, short, apically spoon-shaped; segment 6 short, 
apically narrowing abruptly. 

Peraeopod 3, coxa rectangular, basis, hind margin setose 
throughout; segment 4 broadening gently distally, hind mar- 
gin setose throughout; segment 5, anterior margin with 
proximal excavation or notch, hind margin proximally with 
plumose setae; segment 6 lenticular, marginal spines strong. 
Peraeopod 4, coxa rounded anteriorly, with squared hind 
comer; basis with antero- and postero-distal clusters of setae; 
segment 4, hind margin with 5 setae, 3 longish; segment 5, 
anterior margin with single setal cluster, hind lobe medium, 
antero-distal spine cluster strong, distal margin bare; seg- 
ment 6 small, short, with hind margin and apical spine 
clusters. 

Peraeopod 5, coxa deep, hind margin strongly setose; 
basis asymmetrically broad, hind margin distally bare; seg- 
ment 4 broadening distally, with strong marginal and facial 
spine clusters, and strong postero-distal setal cluster; seg- 
ment 5 narrower, squarish, with stout spine clusters; segment 
6 medium, with 1 anterior marginal spine cluster, and a few 
posterior marginal and apical spines. Peraeopod 6, basis 
relatively short and very broad, broadest distally, hind mar- 
gin short-setose; basis large, broadening distally, with strong 
anterior facial clusters and posterior facial row of spines; 
segment 5 broadest distally with 2 strong anterior facial spine 
clusters; antero-distal margin with 9-10 spines, excavation 
deep; segment 6 large, bent forward, hind margin with 5 
spine clusters, some distal spines elongate, tips funnel shaped, 
notched. Peraeopod 7, basis very broad, proximally truncate 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 


49 



FIG. 9. Eohaustorius robustus (Gurjanova). Female (7.0 mm). Greater Kurile Islands. 
(modified from Gurjanova, 1962). 


behind, margin smooth; segment 4 short, very broad, hind 
lobe narrow, with apical cluster of plumose setae; segment 6 
short, very broad, with 2-3 anterior marginal, and 3 posterior 
marginal spine groups . Longest anterior marginal spines of 
segments 4-6 are club- or funnel-tipped. 

Pleon side plate 3 with a few facial and submarginal 
plumose setae; hind corner moderately produced, acute, 
apex upturned slightly. Uropod 1, rami and peduncle 
subequal, both rami with distally hooked apical spines; outer 
ramus with weak subapical setae, inner ramus, posterior 
margin with 3 groups of long setae. Uropod 2 rami shorter 
than peduncle, normally setose. Uropod 3, rami short, less 
than 2X peduncle; terminal segment of outer ramus very 
short (1/4 proximal segment); inner ramus, inner margin 
with 5-6 stout plumose setae. 


Telson lobes medium, narrowing distally, with about 7 
dorso-distal setae. 


Distribution. Pacific coast of the Large Kurile Island 
chain (Paramushir, Iterup Islands), and sublittoral of the 
northwestern Sea of Okhotsk, at depths of 10-40 m. 

Taxonomic commentary. Another species of the ad- 
vanced subgroup (including £. cheliferus), but distinguished 
by characters given in the key (p. 37). It is not at all closely 
related to E. eous, from which it is distinguished by a 
combination of 3-4 species level character states. E. rob- 
ustus is superficially close to E. gurjanovae in several char- 
acter states of peraeopods 5-7. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 


50 


Eohaustorius brevicuspis, Bosworth 

(Fig. 10) 

Eohaustorius brevicuspis Bosworth, 1973: 255, figs. 1-3. 
—Austin, 1985: 605.— Staude, 1987; 383, 372 (key).— 
Barnard & Karaman, 1991; 363. 

Material examined. 4 lots containing 20 specimens, 
none from British Columbia. 

WASHINGTON. 

ELB Stn W39, Neah Bay, Clallam Co., medium sand at LW, 
July 30, 1966 - 3 males, 2 females, 1 im. NMCC1991-1233; 
ELB Stn. W46, Leadbetter Pt., Pacific Co., surf exposed sand 
atLW, Aug. 4, 1966 - 4 males, 2 females, NMCC 199 1-1236. 

OREGON. 

ELB Stn. W58, Seal Rock, Lincoln Co., LW surf sand, Aug. 
13, 1966 - 1 female ov (4.5 mm) (slide mount) (figured 
speci-men), 1 female ov (4.6 mm) slide mount, CMN Cat. 
no. NMCC 199 1-1237; 4 males, 5 imm. 

CALIFORNIA. 

ELB Stn. Cl, Crescent City, surf sand beach at LW - 1 
subadult female, NMCC 199 1-2094. 

Diagnosis. Female ov(4.0 mm): Head, rostrum short, 
blunt, not exceeding antero-lateral head lobes. Eyes small 
ovate, adjacent to anterior margin, whitish, lacking pigment. 
Antenna 1, peduncular segment 2 with strong anterior mar- 
ginal clusters of setae. Antenna 2, peduncular segment 4 
short, medium deep, hind margin with relatively few ( 1 8-20) 
plumose setae, postero-distal lobe short; segment 5 little 
broadened distally. 

Mandible, palp segment 3 medium long, with 12 poste- 
rior marginal cohib spines. Maxilla 1 & 2?? Maxilliped, 
outer plate medium; palp segment 2, inner lobe relatively 
small, distinctly exceeded by broadly expanded palp seg- 
ment 3. 

Coxa 1?, coxa 2 rounded below. Gnathopod 1, basis, 
anterior margin proximally with short setae, posterior mar- 
gin distally with a few long setae; segment 5 long, deep; 
segment 6 short, distally slightly broadening. Gnathopod 2, 
basis, anterior margin medially setose, posterior margin with 
a few longish setae; segment 4 slender, shallow; segment 6 
short, not medially broadened. 

Peraeopod 3, basis, anterior and posterior margins distally 
with a few long setae; basis medium broad distally, hind 
margin sparsely plumose-setose, segment 5 shallow, with 
postero-proximal marginal setae; segment 6 small, lenticu- 
lar, margins spinose. Peraeopod 4, coxa very broad, lower 
margin nearly straight; segment 4, anterior margin with 2 
small groups of setae, hind margin with pair of long plumose 
setae; segment 5, anterior marginal oblique spine row strong, 
posterior lobe medium, hind margin proximally with a few 
spines and setae, distal margin with weak spine cluster; 
segment 6 medium, anterior margin with 2 weak clusters of 


spines and setae, hind margin distally to apex with a few 
longish setae and medium spines. 

Peraeopod 5, coxa shallow, hind lobe, lower margin 
setose; basis broader than deep, hind margin setose through- 
out; segment 4 slightly broadening distaUy, anterior clusters 
and posterior rows of facial spines strong; segments slightly 
narrower, facial spines strong; segment 6 medium, with 2 
anterior marginal spine clusters, posterior margin with single 
spines. Peraeopod 6, basis broadening distally, with large 
postero-distal lobe, hind margin setose proximally; segment 
4 very broad distally, with 2 weak facial spine groups; 
segment 5 short, very broad with 1 posterior and 2 anterior 
submarginal facial spine groups, distal margin with 6-7 
spines, distal excavation medium; segment 6, short, thick, 
posterior margin with 6-7 spine clusters, long spines split- 
tipped. Peraeopod 7, basis very broad, suborbicular, hind 
margin nearly bare, with broadly rounded proximal cusp; 
segment 4 short very broad distally, anterior margin with 3 
spine clusters, posterior margin with a few plumose setae 
distally; segment 5 narrower, but wider than long, anterior 
margin with 2-3 spine clusters, postero-distal comer with 
short to medium spines; segment 6 broad, with 1 anterior and 
2 posterior marginal spine clusters and long spines at tmn- 
cate apex. 

Pleon plate 3 , hind comer moderately strongly produced, 
tip acute, not upturned. Uropod 1 , peduncle, outer margin 
with a few distal spines and apical cluster of 3 heavy spines; 
rami with strong apical spine clusters; inner ramus with 
several long posterior marginal setae and a medio-distal 
cluster of spines; outer ramus with a few posterior marginal 
spines; uropod 3, rami subequal, ~'2X peduncle, terminal 
segment of outer ramus medium; inner ramus, inner margin 
with 3-4 plumose setae. 

Telson lobes short, thick, with 7-8 dorsal distal setae and 
several inner marginal setae. 

Distribution. Central California north to the Strait of 
Juan de Fuca, in clean medium sand of surf exposed high 
salinity beaches, MW level to immediate subtidal depths. 

Taxonomic commentary. E. brevicuspis is closely 
similar to the intertidal species washingtonianus, overlap- 
ing it distributionally in the Oregon- Washington region, and 
replacing it further south. 

Eohaustorius washingtonianus (Thorsteinson) 
(Figs. 11, 12) 

Haustorius washingtonianus Thorsteinson, 1941:61, figs. 
39-51. 

Eohaustorius washingtonianus J.L. Barnard, 1957: 81 (part). 
— Barnard, 1962: 249 (key). — Bosworth, 1973: 8 (key), fig. 
E.— Austin, 1985: 607.— Staude, 1987: 383, 372 (key).— 
Barnard & Karaman 1991: 363. 

non : Eohaustorius washinstonianus Barnard, 1957: PI. 16. 
— Gurjanova, 1962: fig. 135A. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 51 



FIG. 10. Eohaustorius brevicuspis Bosworth, 

Material examined. About 55 lots containing approx. 

600 specimens, of all sexes and life stages (except very 
juvenile), as follows (numbers of specimens in parentheses): 

SOUTHEASTERN ALASKA. 

Prince William Sound to Alexander Archipelago, ELB stns . , 
June-Aug., 1961, LW and shallow sub-tidal levels - A54 (3); 
A71 (1); A81 (30); A83 (1); A121 (1); A140 (1). ELB Stns, 
July 28 - Aug. 4, 1980: S4B1 (l);S4B2(f.w. stream outflow) 
(2); S11B3 (15); S16B1 (1); S16B4 (2); S19B1 (2); S16B4 


BRITISH COLUMBIA. 

Queen Charlotte Islands, ELB Stns, July- August 1957- H3 
(1); H8a (2); H13 (29); H14 (17); El (12); E14b (31); E17 
(4); E21 (1); W2 (44). 

North-central mainland coast, ELB Stns, July, 1964: HI (3); 

HIO (1 1): H23 (48); H39 (15); H48 (32); H50 (49); H59 (3). 


1973. Female ov (4. 5 mm). Seal Rock, O regon. 

Northern Vancouver I. & adjacent mainland; ELB Stns 
1959: N1 (15); N6 (16); 013 (1). 

Central Vancouver I., ELB Stns 1975; P28 (48); P29 (1). 
Southern Vancouver L, ELB Stns., 1955: F4, Albert Head, 
near Victoria (2); F5 (9); P6a (8); P8 (4). ELB Stns., July,’ 
1970: P703 (4); P708 (22); P711 (17); P716 (5); P17 (1). 
ELB Stns., 1964: H41 (16); H42 (16); H43 (79); H45 (25). 
ELB Stns., 1975: Plc(15); Plb (46). ELB Stns., 1976: B 12a 
(2); ELB Stns, 1977: B5a, Witty’s lagoon - 1 female ov (7.0 
mm), female ov (5.0 mm), male (5.0 mm) (slide mounts), -i- 
14 additional females, CMN Cat. no. NMCC1991-2107- 
B5c (51). 

Southern mainland, ELB Stns., 1955: Mil, White Rock 

( 10 ). 

WASHINGTON 

ELB stations, 1966: W34, Crescent Beach, LW sand (with£ 

estuarius) - 10 males, 19 females, 5 im. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 52 


Diagnosis. Female (5.0 mm): Head, rostrum short. Eyes 
small, lenticular, whitish, lacking pigment. Antenna 1, 
segment 2 with strong anterior marginal setae, lacking 
proximally. Antenna 2, segment 4 medium deep, hind 
margin with ~25 plumose setae, postero-distal lobe medium; 
segment 5 large, medium broad; flagellar segment 1 with 
single postero-distal plumose seta. 

Mandible, palp segment 3 medium, with 11-12 posterior 
marginal comb spines. Maxilla 1, palp segment 1 short. 
Maxilla 2, inner plate with inner marginal setae only. 
Maxilliped, inner plate and outer plates broad; palp segment 
2, medial lobe broad, not attaining tip of moderately broad- 
ened segment 3. 

Coxa 1, and 2 small, squarish. Gnathopod 1, basis with 
few distal posterior marginal setae; segment 5 medium deep; 
segment 6 broadening distally. Gnathopod 2, basis with 
postero-distal marginal setae; carpus slender, elongate, 
postero-distal spines slender; segment 6 short, medially 
broadest. 

Peraeopod 3, basis medium, hind margin with distal 
setae; segment 4 long, gently broadening distally; segment 5 
medium deep, anterior margin with shallow proximal exca- 
vation, hind margin proximally with setae; segment 6 drop- 
shaped, margins slender-spinose. Peraeopod 4, segment 6, 
hind margin with 2-3 long plumose setae; segment 4 with 
strong anterior marginal oblique row of spines, hind lobe 
medium, with 2 postero-proximal, and 1 distal, spine cluster; 
segment 6 slender, with 2 anterior groups of spines and setae, 
and hind margin distally with single spines and setae. 

Peraeopod 5, coxa, hind lobe deep, margin weakly setose; 
basis short broad, suborbicular, hind margin setose except 
distally; segment 4 short, broadest distally, With moderate 
anterior clusters and posterior rows of facial spines; segment 
5 longer than wide, facial spines strong; segment 6 slender, 
with 2 anterior marginal and 3 posterior marginal clusters of 
slender spines and setae, apex slender-spinose. Peraeopod 6, 
coxa deep, hind lobe setose below; basis broad, with shallow 
distal lobe, hind margin setose proximally ; segment 4 medium 
long, broadest distally, with 2 weak facial spine clusters; 
segment 5 broadest distally, with 2 medium posterior facial 
clusters of spines and distal marginal row of 8-10 spines, 
distal excavation medium; segment 6 medium, nearly straight, 
hind margin with 5-6 clusters of spines, a few distal spines 
long, split-tipped. Peraeopod 7, basis broad, suborbicular, 
hind margin nearly bare, with strong proximal cusp or tooth; 
segment 4 medium, widest distally, hind margin setose 
throughout; segment 5, anterior margin with 2 clusters of 
spines, tips clavate, distal free margin with small spine 
cluster; segment 6 medium broad, with 1 antero-marginal 
and 2 postero-marginal clusters of spines. 

Pleon plate 3, hind comer weakly produced, acute, well 
exceeded by postero-dorsal pleosomal lobe. Uropod 1, 
peduncle with a few weak marginal spines, distally with 3- 
4 stout spines; rami subequal; inner ramus, posterior margin 
setose; outer ramus posteriorly with singly inserted and 
clusters of spines and setae. Uropod 3, outer ramus, terminal 


segment medium; inner ramus with 4-5 inner marginal 
plumose setae. Telson lobes short, thick, with 5-6 dorso- 
distal and 4-5 inner marginal setae. 

Distribution: From Prince William Sound, Alaska, 
southward along southeastern Alaska, British Columbia and 
Washington to southern Oregon, possibly to central 
California. It occurs bathymetrically from about mid-tide to 
shallow sub-tidal levels, in fine sand, mainly along open, 
surf-exposed beaches, but also on protected beaches; it co- 
occurs with E. estuarius in salinities as low as - 10%o. 

Taxonomic commentary: E. washingtonianus is the 
type of a unique and moderately advanced N. American 
endemic group of species. It contains 3 other N. American 
endemic full species, as noted in the key, and a variety as 
noted below. The group is typical of high energy intertidal 
surf sands, but the subtidal members are less strongly ar- 
moured. This species complex is most closely related to £. 
eous group of western Pacific shores. As noted by Gurjan- 
ova (1962), it bears some resemblance to, and possible direct 
relationship with, E. gurjanovae (see histogram, p. 59). 


Eohaustorius washingtonianus variant 

Material examined. 

BRITISH COLUMBIA. 

North-central coast. ELB Stns., 1964: H48, Goose I., north 
beach, fine sand at LW level, 9.8 C., Aug. 5-17 males, 14 
females, 1 immature. ELB Stns., 1959: Nl, Open Bight, 
Rivers Inlet, coarse sand atLW level, Aug. 3-15 im., CMN 
Cat. no. NMCC 1991 -2095 ;N6,Bremner Beach, near Raynor 
Pt., fine sand at LW level, 10.0 C., Aug. 6 - 7 males, 9 
females. 

Taxonomic commentary. Bos worth (personal com- 
munication) briefly commented upon a somewhat anom- 
alous feature of specimens of "washingtonianus" from the 
three stations listed above. This observation is here con- 
firmed. In peraeopod 7, segment 2 (basis) bears a small but 
distinctpostero-proximal cusp, typical of £. washingtonianus, 
£. brevicuspis and£. bamardi of N.orth American beaches, 
and £. gurjanovae of western Pacific shores (p. 47). However, 
the present variant resembles £. bamardi in having a single 
group of spines (excluding the antero-distal group) on the 
anterior margin of segment 5 of peraeopod 7. This northern 
variant differs from £. bamardi in its other specific char- 
acters (key, p. 37), but appears otherwise similar to material 
of washingtonianus from adjacent northern localities. We 
therefore conclude, tentatively, and on the basis of the 
limited material available, that specimens from the three 
stations above represent a local, mainly subtidal, variant of 
the typical form of Eohaustorius washingtonianus 
(Thorsteinson). 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 53 




AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 54 



FIG. 12. Eohaustorius washingtonianus (Thorsteinson). Female (5.5 mm). Point Roberts, WA. 

(after Thorsteinson, 1941). 


Eohaustorius barnardi , new species 
(Fig. 13) 

Eohaustorius washingtonianus J. L. Barnard, 1957; 82, plate 
16. — Bosworth, 1974 (letter and manuscript to ELB). 

Material. The species occurred in samples from the 
1956 and 1959 “Velero” cruises near Pt. Conception, and 
further south, in depths of 5-20 meters (Barnard, loc. cit.). 

The species was also collected by E. W. Fager from the 
end of the Scripps’ s pier in 1955- 1956 (fide W. S. Bosworth). 

Diagnosis. Female ov., Holotype (5.0 mm), 5 Paratype 
specimens, ’’Velero" Stn. 2312-53, collections of the Allan 
Hancock Foundation. Similar to Eohaustorius washington- 
ianus, with the following differences: 

Mandible, palp segment 3, posterior margin with 9-10 
(vs. 1 1) comb spines, and distal spines of outer margin more 
numerous (9-10 vs. 6-7). Maxilla 2, outer plate with 1 distal 
outer marginal plumose seta. Maxilliped, outer plate shorter, 
more slender; palp segment 3 less broadly expanded. 

Gnathopod 1 , segment 5 more deeply broadened distally . 
Gnathopod 2, basis, hind margin more heavily setose; seg- 
ment 6 broadened distally. 

Peraeopod 3, coxa, antero-distally angled, not rounded, 
lower margin nearly straight. Peraeopod 4, coxal plate 
subrectangular; segment 5, hind lobe short; segment 6 broad- 
ened medially. 

Peraeopod 5, coxa shallower, hind lobe more richly 
setose behind; basis less broad; segment 6 relatively short 
broad, margins and apex with fewer spines. Peraeopod 6, 


basis broadening distally; segment 4 slightly narrowing 

distally, facial spines few, weak; segment 5, facial spines 
few, distal excavation more pronounced. Peraeopod 7, basis 
with weaker proximal posterior cusp; segment 4 less broad 
distally; segment 5, anterior margin with 1 cluster of spines. 

Pleon plate 3, hind comer more strongly produced, 
sharply acute, less exceeded by postero-dorsal process of 
pleon 3. Uropod 3, rami more slender, inner ramus with 
fewer inner marginal setae. 

Taxonomic commentary. According to Bosworth 
(1973; personal communication), Barnard (1957, plate 1) 
incorrectly designated his subtidal material from southern 
California as Eohaustorius washingtonianus, mainly be- 
cause of the pronounced cusp on the basis of peraeopod 7. 
However, Bosworth noted that the cusp is more strongly 
pronounced, and the ratio of segments 5 & 6 of peraeopod 5 
is different in Thorsteinson's original northern species. 

Other differences, noted in this study, include (in E. 
barnardi) the smaller size of maxilliped palp segment 3, the 
smaller size of the carpal lobe of peraeopod 4, the weaker 
facial armature of segments 4 & 5 of peraeopod 6, the less 
prominent hind lobe of segment 4 of peraeopod 7, and the 
more prominent and more strongly angled posterior process 
of pleon plate 3. 

Etymology. We take pleasure in formally naming this 
species in honour of the late Dr J. L. (Jerry) Barnard who 
intially described and figured it, and who contributed inesti- 
mably to the advancement of knowledge of the systematics 
and biogeography of fossorial amphipod crustaceans. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 55 



MX2 MX1 

FIG. 13. Eohaustorius barnardi, new species. Female (5.0 mm). San Pedro shelf, --15 m, California. 

(modified from Barnard. 1957L 


Eohaustorius cheliferus (Bulycheva) 

(Fig. 14) 

Haustorius cheliferus Bulycheva, 1952: 198, fig. 3. 
Eohaustorius heliferus Gurjanova 1962; 411, figs. 138 A, B. 
Eohaustorius cheliferus Barnard & Karaman, 1991; 363. — 
Ishimarus, 1994; 64. 

Diagnosis: Female ov (7.0 mm) Head broad, rostrum 
short, broadly acute. Eyes unpigmented. Antenna 2, pedun- 
cle 4, posterior lobe large, with 35-t- marginal plumose setae, 
postero-distal lobe strongly produced, attaining end of seg- 
ment 5; segment 5 broadest medio-distally; flagellar seg- 
ment 1 with 3 postero-distal plumose setae. 

Mouthparts imdescribed. 

Gnathopod 1, basis, hind margin weakly setose; seg- 
ment 5 shallow, not elongate; segment 6 broadest medio- 
distally, dactyl stout, unguis linear, longer than body. 
Gnathopod 2, basis, posterior margin distally setose; seg- 
ment 5 slender, postero-distal spines each with medial cross- 
piece, distally toothed; segment 6 slender, short. 

Peraeopod 3, coxa lunate, hind comer acute; basis 
broad, margins distally setose; segment 4 medium, distally 
broad, hind margin richly setose; segment 5 deep, hind 
margin heavily setose; segment 6 drop-shaped, margins 
lightly spinose. Peraeopod 4, segment 4, anterior oblique 


row with stout spines, posterior margin with 3 long setae; 
segment 5 with strong anterior oblique spine row, posterior 
lobe large, long, postero-proximal margin with 4 clusters of 
spines and long setae, distal free margin bare; segment 6 
small, overhung by lobe of 5, with single anterior marginal 
spine cluster, posterior marginal spines continuous with 
apical spines. 

Peraeopod 5, basis broadening distally, postero-distal 
lobe faint, hind margin fully setose; segment 4 long, little 
broadened, facial spine rows strong; segment 5 subquadrate, 
facial spines strong; segment 6 medium, with single anterior 
and posterior marginal spine groups. Peraeopod 6, basis 
broad, hind margin strongly convex, setose proximally; 
segment 4 medium, broadest subapically, with 4-5 clusters 
of facial spines; segment 5 slightly broader distally, with 
single facial spine cluster, distal free margin with 7-8 spines, 
distal excavation medium deep; segment 6 short, curved 
forwards, hind margin with longish simple-tipped spines. 
Peraeopod 7, basis broad, hind margin nearly straight, distally 
weakly setose, lacking proximal cusp; segment 6 triangular, 
broadest distally, hind margin setose; segment 5 longer than 
broad, anterior margin with 2-3 spine clusters, distal free 
margin short; segment 6 medium broad, anterior margin with 
1, posterior margin with 2, spine clusters 

Pleon plate 3, hind comer acute, produced, apex acute 
slightly angled upwards; lower margin setose. Uropod 3, 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 56 



FIG. 14. Eohaustorius cheliferus (Bulycheva). Female ov (7.0 mm). Japan Sea to Sea of Okhotsk. 

(modified from Bulycheva, 1952) 


rami medium; terminal segment of outer ramus medium; 
inner ramus, inner margin with 4-5 plumose setae. Telson 
lobes elongate, narrowly oval, with long dorso-distal setae. 

Distributional commentary. Pacific coast of Iturup I, 
30-40 m depth. Also recorded from the Sea of Japan (Peter 
the Great Bay) in depths of 0.75-13 m; also Sea of Okhotsk 
(Amur R. estuary and Aniv Bay) and Southern Kurile Strait, 
in depths of 6 - 40 m (Gurjanova, 1962). 

Taxonomic commentary. The illustrations of Buly- 
cheva (1952), repeated in Guijanova (1962), are limited in 
detail but, in conjunction with her descriptive text, provide 
sufficient basis for reliable separation as a species distinct 
from all others of this study. As noted in the phenogram (p. 
59) the species bears similarities to E. longicarpus of South 
Korean waters, and to E. sencillus of the North American 
Pacific coast, but is otherwise distinct from nearly every- 
thing else. 

This species name may encompass a complex of closely 
related species. All materials listed by Gurjanova (1962) 
might therefore be re-examined for this possibility. 


Eohaustorius longicarpus, new species 
(Fig. 15) 

Material examined. 

Pusan, South Korea, protected and beach at LW, Jae-Sang 
Hong coll., June, 1983. - Female ov (4.0 mm) Holotype 
(slide mount); male (4.7 nun). Allotype (slide mount); 
female ov. (3. 5 mm ), Paratype. CMN Cat. no. pending. 

Diagnosis. Female ov(4.0mm); Head, rostrum. Eyes. 
Antenna 1, peduncle 1, anterior margin proximally bare. 
Antenna 2, peduncle 4, hind lobe deep, margin with 20-25 
plumose setae, postero-distal lobe large; segment 5 medially 
deepest; flagellar segment 1 with 1-2 postero-distal setae. 

Mandible, palp segment 3 slender, posterior margin 
with 10 comb spines. Maxilliped, inner plate broad medi- 
ally; outer plate large, broad but short; palp segment 2, inner 
lobe broad, large, extending almost to tip of slender seg- 
ment 3. 

Coxae 1 & 2 small, medium deep. Gnathopods 1 & 2 
generally similar to those of E. cheliferus. 

Peraeopod 3 ordinary. Peraeopod 4, coxa relatively 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 57 



FIG. 15. Eohaustoriuslongicarpus,ney,s^dts. South Korea. Male (4.5 mm); female (4.0 mm). 


narrow, deep; basis slender, lacking distal setae; segment 4 

with weak anterior oblique spine cluster, hind margin with 3 
long plumose setae; segment 5 with anterior oblique row of 
slender spines, hind lobe elongate, proximal margin with 3 
spine clusters, distal free margin bare; segment 6 slender, 
nearly exceeded by hind lobe of segment 5, anterior margin 
with 1, posterior margin with 2-3, groups of slender spines 
and setae. 

Peraeopod 5, hind lobe of coxa narrow, deep, hind 

margin strongly setose; basis relatively slender, subovate. 


lacking distinct postero-distal lobe; segment 4 short, uni- 

formly broad, facial spine rows strong; segment 5 broader 
than long, facial spines strong; segment 6 broad, anterior 
margin with 3-4 singly inserted or groups of spines, hind 
margin distally with 2 slender spines. Peraeopod 6, basis 
little expanded distally broadest, with weak distal lobe, hind 
margin distally bare of setae; segment large, long, broad 
throughout, with 5-6 clusters of facial spines; segment 5 
short, very broad distally, with 1 or 2 facial spines, and 5-7 
distal margin spines, distal excavation very shallow; seg- 


AMPHIPACMCA VOL. 11 NO. 1, AUG. 31, 1995 58 


ment 6 straight, hind margin with 6-7 spines, long spines 

simple. Peraeopod 7, basis medium broad, hind margin 
nearly straight, nearly bare, lacking proximal cusp; segment 

4 triangular, broadest distally, hind margin setose; segment 

5 subquadrate, anterior margin with 2 spine groups, distal 
free margin with 1-2 small spine groups; segment 6 medium, 
broadest medially, anterior margin with 1, posterior margin 
with 3, clusters of slender spines. 

Pleopods, peduncle large, broad; outer ramus with 15? 
segments, inner with 10 segments? Pleon plate 3, hind 
comer strongly produced, sharply upturned near apex, base 
of inner margin with 3 long setae. Uropod 1, rami subequal; 
peduncle, outer margin nearly bare, with 2-3 weak distal 
spines; inner ramus, posterior margin with 2 setae; outer 
ramus with a few posterior marginal spines. Uropod 3, rami 
relative short, thick, terminal segment long; inner ramus, 
inner margin with 4 long setae. Telson lobes short, thick, 
with 5-6 dorso-distal and a few inner marginal setae. 

Coxal gills short, saclike 

Etymology. From longi - + -karpos (wrist), alluding to 
the elongate posterior lobe of the carpus of peraeopod 4. 

Distribution. Known only subtidally from sand beaches 
in South Korea. 

Taxonomic and biogeographical commentary. The 

species exhibits mainly pleisiomorphic character states, and 
clusters generally with the primitive E. eous complex (F.g. 
16, p. 59). It is not closely related to any other species (well 
below 75% similarity levels) and the mjterial is regrettably 
insufficient for biographic commentary. 

Discussion and Conclusions 

In this study, the genus Eohaustorius was found to en- 
compasses 1 3 described species that are endemic to intertidal 
and shallow subtidal waters of the North Pacific marine 
region. Their sediment-burrowing and filter-feeding life 
styles are accompanied by limb adaptations that are grossly 
similar to, but much more highly specialized than, those of 
members of the North-Pacific endemic talitroidean family 
Dogielinotidae from which they are now phyletically 
separated (Bousfield & Tzvetkova, 1982; Barnard & 
Karaman, 1991). However, members of the Dogielinotidae 
are more advanced phyletically in having strongly sexually 
dimorphic gnathopods, and utilizing pre-amplexing 
reproductive behaviour (Bousfield & Shih, 1994). 

As noted previously (e.g. Barnard, 1957; Bousfield 
1 965), Eohaustorius is grossly similar in body form and limb 
structure to the 7 other genera of family Haustoriidae most 
of whose member species are endemic to the North American 
Atlantic region (Bousfield, 1970). However, the species of 
Eohaustorius are distinguished not only by their generally 
smaller size, but by their less highly specialized mouthparts, 
smaller coxae of gnathopods 1 &2,unUke formofperaeopods 
3 & 4, generally shorter, broader, and less spinose distal 


segments of peraeopods 5-7, lack of a distal ventral lappet on 

urosome 1, more setose rami of uropod 3, and the widely 
separated (basally unfused) lobes of the telson, among other 
differences. 

Concerning a common ancestry for these 8 genera, Eo- 
haustorius appears least different from the genus Pseudo- 
haustorius Bousfield, 1965. Similar character states include 
those of: (1) antennae 1 & 2 (flagella short, few segmented); 

(2) maxilla 1 (weakly setose inner plate, lack of baler lobe); 

(3) maxilla 2 (plates relatively unmodified for filter feeding); 

(4) maxilliped palp (segment 3 claviform); (5) peraeopod 6 
(segment 6 spatulate [vs. linear]); (6) pleon segment 3 
(strongly produced dorso-distally, lateral plate acutely 
produced); (7) urosome 1 (peduncle and rami setose, weakly 
spinose); (8) urosome 2 (nearly occluded dorsally by urosome 
segments 1 & 3); (9) uropod 3 (terminal segment of outer 
ramus short) and (10) telson (lobes setose [vs, spinose]). 
Some of these character states (e.g., 6, 10), as well as the 
subrectangular form of segment 5 of peraeopod 6, are typical 
also of the genus Acanthohaustorius. Whether these sim- 
ilarities signify relatively close phyletic relationships or 
accrue mainly to similarities in lifestyle and habitat of com- 
ponent species is moot. If phyletic, morphological similarities 
would link two genera that appear to have little readily dis- 
cernible biogeographical relationship (see p. 59). An 
alternative possibility, that the genus Eohaustorius evolved 
independently from a pontoporeiid ancestral group, and that 
the family Haustoriidae is therefore polyphyletic, receives 
little support from this analysis. 

Within the genus Eohaustorius, numerical analysis of 
20 selected morphological characters and pertinent character 
states of 12 of the 13 described species is summarized in a 
phenogram of species similarities (Table I; Fig. 12). The 
present modification of the UPGMA cluster analysis system 
of Sneath & Sokal (1973) has been used in similar studies of 
other North Pacific amphipod groups (e.g., Conlan, 1983; 
Jarrett & Bousfield, 1994). Here the analysis is slightly 
compromised by limited morphological information available 
concerning mouthparts of some western North Pacific species. 
Despite the unavoidable emphasis on character states that 
may reflect burrowing behaviour rather than phyletic relat- 
ionships, the overall results are considered significant. 

In the phenogram (Fig. 16) three main groups "cluster 
out" at better than 60% similarity levels. In the centre is a 
relatively primitive eous group of six species, from both Asi- 
atic andNorth American coastal regions, having P.-A. indices 
mainly of 13-16, but 23 for the somewhat isolated E. sen- 
cillus. The core group is flanked on the left by the somewhat 
aberrant Asiatic cheliferus group, with P. -A indices of 13- 
20, and on the right by the North American washingtonianus 
group, with P. A. Indices of 16-22. The cheliferus group is 
characterized by strongly produced and/or distally hooklike 
hind comer of pleon plate 3 relatively strongly spinose hind 
margin of segment 6 of peraeopod 5, slender telson lobes, 
low numbers of comb spines on mandibular palp segment 3, 
and well-developed hind lobe of segment 5, peraeopod 4. 
Members of the washingtonianus group have a proximal 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31. 1995 59 


40 
38 
> 36 

H- 

j 32 


® 30 

O) 

28 

UJ 

< 26 
So 24 
22 


FIG. 16. PHENOGRAM OF NORTH PACIFIC SPECIES OF EOHAUSTORIUS* 

abcdefghjklm 


cc 

LU 

I- 

o 

< 

cr 

< 

X 

o 

Q 

UJ 

X 

< 

Q. 


20 

18 

16 

14 

12 

10 

8 


"r 

13 


"T" 

20 


I I 

17 13 


"T- 

14 


"T" 

13 


16 


-T" 

15 


23 


"r 

16 


SPECIES 

A subulicofus 

B cheliferus 

C robustus 

D gurjanoyae 
E eetuarius 

F ecus 


G 

H 

J 

K 

L 

M 


"r 

16 


sawyer/ 

longicarpus 

senci/lus 

wastiingtonianua 

brevicuspis 

barnardi 


22 P.-A. INDEX 


75 


>- 

X 

< 


50 


CO 


25 


* except. E. tandeensis Dang, 1968 


cusp on the posterior margin of the basis of peraeopod 7, one 
spine cluster on the postero-distal margin of segment 5 of 
peraeopod 4, and a relatively large maxilliped palp segment 
3. The core eous group shows mainly plesiomorphic char- 
acter states, including a relatively elongate, facially and 
marginally spinose, segment 4 of peraeopod 6 that typifies 
most Atlantic genera of haustoriinids. E. sencillus is 
uniquely advanced in its very short antennal flagella, enlarged 
dactyl of gnathopod 1, and short maxilliped palp segment 3. 
All in all, few species pairings exhibit greater than 75% 
similarity and none is closely related, suggesting long peri- 
ods of isolation and limited gene flow between populations. 
The relatively primitive nature of intertidal vs. subtidal spec- 
ies of Eohaustorius is consistent with similar trends in other 
regional fossorial amphipods (e.g, Jarrett & Bousfield, 1 994a). 


Biogeographical Considerations 

The subregional occurrence of species of Eohaustorius 
is provided in Table II. Of the twelve species considered 
here, five are endemic to Asiatic North Pacific shores, and 
six to the North American coast. Only one species, E. eous, 
occurs in both continental waters, and only in the Bering Sea 
region. 

In the Asiatic region, E. robustus and E. cheliferus are 
confined mainly to the Sea of Okhotsk and Kamchatka 
regions whereas E. gurjanovae, E. longicarpus and £. sub- 
ulicolus have been recorded exclusively or mainly from 
southern Sakhalin Island and the Sea of Japan. In the more 
southerly region, these haustoriid species overlap distri- 
butionally, in similar sedimentary habitats, with members of 
the talitroidean fossorial family Dogielinotidae. The dogiel- 


AMPHIPACIFICA VOL. 11 NO, 1, AUG. 31, 1995 60 


TABLE I. CHARACTERS AND CHARACTER STATES OF SPECIES OF EOffAl/SrO/f/l/S 



CHARACTER STATE VALUE 

CHARACTER 

Plesiomorphic 

0 

Intermediate 

1 

Apomorphic 

2 ■ 

1. Antenna 2, peduncle 4, number of 

<20 

25 

>30 

posterior marginal setae 




2. Antenna 2, flagellar segment 1, 

1 

2 

3+ 

number postero-distal long setae 




3. Mandibular palp segment 3, number of 

10+ 

7 

5 

posterior marginal comb spines 



Small 

4. Maxilliped palp, segment 3, size 

Large 


5. Peraeopod 3, coxal shape 

Squarish 


Semilunate 

6. Peraeopod 4, hind lobe of segment 5 

Short 

W>L 


Long 

L»W 

7. Peraeopod 4, segment 5, hind lobe, 

Absent 


Present 

distal marginal spines 




8. Peraeopod 5, length of segment 4 

Long 


Short 

9. Peraeopod 5, shape of segment 5 

Narrow 


Wide 

10. Peraeopod 5, segment 6, number 

2-3 


1 

of posterior marginal spines 




11. Peraeopod 6, length of segment 4 

Long 

L»W 


Short 

W=L 

12. Peraeopod 6, segment 5, number 

2 


1 

of anterior marginal spine clusters 




13. Peraeopod 6, segment 4, hind 

1+ 


0 

marginal spines 




14. Peraeopod 7, basis, proximal hind 

lacking 


present 

marginal cusp 




15. Peraeopod 7, segment 5, number 

2-3 


1 

of anterior marginal spine clusters 




16. Peraeopod 7 segment 6, number 

3-4 

2 

1 

of posterior marginal spine clusters 




17. Pleon plate 3, type of hind process 

short 

medium 

straight 

long, hooked 

18. Uropod 1, inner ramus, number of 

5+ 

2 

0 

posterior marginal setae 




19. Uropod 3, size of terminal seg- 

Long 


short 

ment of outer ramus 




20. Telson lobes, form. 

elongate 


short 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 61 


TABLE II.. DISTRIBUTION OF NORTH PACIFIC SPECIES OF EOHAUSTORIUS 


SPECIES 

BIOGEOGRAPH 

I CAL ZONES 


1 

2 

3 

4 

5 

6 

7 

8 

9 

E. subulicolus'^ 

X 









E, longicarpus^ 

X 









E, gurjanovae^ 

X 

X 








E, cheliferus^ 

X 

X 








E, robustus^ 


X 








E. eous^ 


X 

X 







E, estuarius* 




9 

X 

X 

X 

9 


E. washingtonianus* 




X 

X 

X 

X 

X 


E. brevicuspis* 






X 

X 

X 


E. sawyeri* 






X 

X 

X 

X 

E. sencillus^ 







X 

X 

X 

E. barnardi^ 








X 

X 


ZONES: 1. Japan Sea and southward 2. Sea of Okhotsk region 3. Bering Sea -W.Alaska 
4. Southeastern Alaska 5. Northern British Columbia 6. Southern British Columbia 
7. Washington-Oregon 8. North & Central California 9. Southern & Baja California 
Ecology:* Intertidal; ^ Subtidal 


inotid species, of similar or slightly larger size, tend to occur 

mainly intertidally, during summer months at least, along 
sandy beaches and in estuaries, often in very high densities 
(Kamihira, 198 1 ; Bousfield & Tzvetkova, 1982). The north- 
ernmost beaches are subject to freezing and ice scour, esp- 
ecially during the winter and early spring, during which time 
the dogielinotids shift from the littoral to the infralittoral 
zone. The regional haustoriid species occur subtidally, at 
least during summer months, and probably year-round. 
Perhaps intense competition with the filter-feeding and “sand- 
licking” dogielinotids in summer, and rigorous physical con- 
ditions in winter, are factors that have apparently prevented 
evolution of Asiatic regional intertidal haustoriid species. 

Along North American Pacific sandy shores however, 
the situation is strongly contrasting. Of the six species 
recorded from southeastern Alaska to southern California, 


the four northernmost species, E. estuarius, E. 
washingtonianus, E. brevicuspis and E. sawyeri occur 
essentially intertidally and shallow sublittorally. As noted 
on page 59, and in figure 16, these northern species show 
mostly plesiomorphic character states and probably evolved 
early during the penetration of the genus into the North 
Pacific region. The two southermost species, E. sencillus 
and E. bamardi, are strictly subtidal and their character 
states are significantly more advanced. However, the 
northern intertidal species and one southern subtidal species 
(£. sencillus) all co-occur in biogeographical zone 6 
(Washington-Oregon), the very region in which the single 
North American dogielinotid species, Probosdnotus loquax 
(Barnard, 1967) occurs intertidally in great abundance 
(Hughes, 1982). '^\^%ptc\^^,dS[d.Eohaustonusbrevicuspis, 
co-occur intertidally on open surf sand beaches and are 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 62 


presumed to be heavily preyed upon by shore birds, especially 
during late summer. However, despite these negative 
factors of competition and predation, intertidal haustoriids 
are able to occur commonly throughout zone 6, and indeed 
zones 4-9, almost certainly because of year-round near 
uniformity of coastal marine conditions; water temperature 
seldom fall below 5®C, and winter ice scour is non-existent 
(Thomson, 1981). These near-uniform physical conditions 
probably account for the relatively wide geographical range 
of the North American species, each of which occurs in 3-5 
biogeographical zones vs. the 1-2 zones of the Asiatic 
species. 

With respect to its overall biogeographical affinities, 
Eohaustorius is essentially a cold temperate genus and, in 
this respect, closer to the presumed para-ancestral ponto- 
poreiid and perhaps distantly ancestral gammaroidean groups 
that are restricted to holarctic regions (Bousfield, 1970; 
Bousfield & Shih, 1994). In the North Pacific, members of 
the genus Eohaustorius occur well north of 60^^ north lati- 
tude, and into the Bering Sea region, but apparently not into 
arctic waters where the Pontoporeiidae dominate (Bousfield, 
1987). In the western North Atlantic region, however, the 7 
haustoriid genera are essentially temperate, and warm- temp- 
erate in thermal requirements. Species of the most eurytopic 
genus, Haustorius, range along North American shores 
north only to latitude 47® (southern Gulf of St. Lawrence) 
where they appear to be limited intertidally by the severity 
and duration of winter conditions (Bousfield, 1965). In 
western Europe, however, where winter conditions are 
relatively mild and reminiscent of those of the western north 
Pacific, the species H. arenarius attains 60® north latitude 
(southern Norway) (Lincoln, 1979). 

In conclusion, we have noted on p. 59 that Eohaustorius 
is grossly similar morphologically to the North Atlantic 
complex of haustoriid genera, but is here found biogeo- 
graphically unrelated to them. In absence of firm evidence 
to the contrary, the genus Eohaustorius is here surmised to 
have been isolated in the North Pacific for a considerable 
period of time. An hypothetical subtidal common ancestor 
may have connected it directly to the relatively primitive 
North Atlantic genus, Pseudohaustorius, possibly during the 
early Miocene epoch. At that time, the Panama isthmus had 
not yet formed and suitably cool marine connections existed 
between Atlantic and Pacific coastal marine regions (Adams, 
1981). Although such an explanation is not entirely 
satisfactory, it does accord reasonably with rationale proposed 
for similar Pacific-Atlantic disjunct distributions in other 
amphipod groups. Thus, in some members of the fossorial 
phoxocephalid genus Eobrolgus (Jarrett and Bousfield, 
1994b) and in two species of the non-substrate modifiying 
parapleustin genus Incisocalliope (Bousfield and Hendrycks, 
1995), the distributional hiatus and its explanation may be 
similar, but the evidence for it appears to be more compelling. 


REFERENCES 

Adams, C.G., 1981. An Outline of Tertiary palaeogeography. 
Ch. 14, pp. 221-235. The Evolving Earth. P. H. Greenwood 
& R. L.M. Cocks (eds.). Brtish Museum Natural History. 
Cambridge University Press. 

Austin, W. C., 1985. An annotated checklist of marine in- 
vertebrates in the cold temperate Northeast Pacific. 
Khoyatan Marine Laboratory, Vol. HI., 1985. 

Barnard, J. L., 1957. A new genus of haustoriid amphipod 
from the northeastern Pacific Ocean and the southern 
distribution of \Jrothoe varvarini Gurjanova. Bull. So. 
Cal. Acad. Sci. 56, Part 2; 81-84, pi. 16. 

, 1962. A new species of sand-burrowing 

amphipod crustacean from Southern California. Bull. 

S. Calif Acad. Sci. 61; 249-252. 2 figs. 

, 1967. New and old dogielinotid marine 

Amphipoda. Crustaceana 13: 283-291, 6 figs. 

, 1975. Amphipoda: Gammaridea. pp. 313- 

366. in Light's Manual (Intertidal invertebrates of the 
central California coast), 3rd edition. R. I. Smith & J. T. 
Carleton (eds.). 716 pp. 

, & M. M. Drummond, 1982. Gammaridean 

Amphipoda of Australia, Part V: Superfamily Haustori- 
oidea. Smiths. Contr. Zool. 360: 1-148, 58 figs. 

, and G. S. Karaman, 199 1 . The Families and 

Genera of Marine Gammaridean Amphipoda (Except 
Marine Gammaroids). Rec. Austral. Mus., Pts. 1 & 2: 866 
pp., 133 figs. 

Bosworth, Jr., W. S . , 1973. Three new species of Eohaustorius 
(Amphipoda: Haustoriidae) from the Oregon Coast. 
Crustaceana, 25: 253-260, 2 figs. 

Bousfield, E. L., 1958. Ecological Investigations on shore 
Invertebrates of the Pacific Coast of Canda. Natl. Mus. 
Can. Bull. 147: 105-115. 

, 1963. Investigations on seashore inver- 
tebrates of the Pacific coast of Canada, 1957 and 1959. 
I. Station List. Natl. Mus. Can. Bull. 223: 49-57. 

, 1965. Haustoriidae of New England 

(Crustacea: Amphipoda). Proc. U. S. Natl. Mus. No. 
3512, Vol. 117: 159-240, 31 figs. 

, 1968. Studies on littoral marine inverte- 
brates of the Pacific coast of Canada. I. Station List. 
Natl. Mus. Can. Bull. 223: 49-57. 

, 1970. Adaptive Radiation in sandburrow- 
ing amphipodcrustaceans. Chesapeake Sciencel 1 (3): 143- 
154. 

, 1973. Shallow-water Gammaridean Am- 
phipoda of New England. Cornell Univ. Press. Ithaca, N. 
Y. 312 pp., 69 pi.. 

— , 1982a. Amphipoda (Palaeohistory). 

McGraw-Hill Yearbook Science & Technology. 1982- 
83: 96-100. 


AMPHIPACIFICA VOL. 11 NO. 1, AUG. 31, 1995 63 


, 1982b. Amphipoda. Gammaridea. in S. P. 
Parker [ed.]. Synopsis and classification of living org- 
anisms. McGraw-Hill, New York, vol. 2: 254-285, and 
293-294. 

, 1987. Revised morphological relationships 
within the amphipod genera Pontoporeia and Gammar- 
acanthus and the "glacial relict" significance of their 
postglacial distribution. Jour. Fish. Aqu. Sci. 46(10)- 
1714-1725. 

, 1990. Morphological Convergence in 

Free-burrowing amphipods and its significance in phyl- 
etic classification. Proc. 5th Amphipod Colloquium, 
Darling Marine Centre, Walpole, Me., September, 1989. 
Oral presentation. Abstr. 

^ , & E. A. Hendrycks, 1995. The amphipod 

family Pleustidae on the Pacific coast of North America: 
Part III. Subfamilies Parapleustinae, Dactylopleustinae 
and Pleusirinae. Sy stematics and Distributional Ecology. 
Amphipacifica II (1): 65 - 134. 

— ^ -, & N. E. Jarrett, 1981. Station Lists of Mar- 

ine Biological Expeditions of the National Museum of 
Natural Sciences in the North American Pacific Coastal 
Region, 1966 to 1980. Syllogeus. Natl Mus. Nat. Sci. 
No. 34: 1-66. 

^ , & D. E. McAllister, 1962. Station list of the 

National Museum marine biological expedition to south- 
eastern Alaska and Prince William Sound. Natl. Mus. 
Nat. Sci. Bull. 183:76-103. 

, and C.-t. Shih, 1994. The phyletic classif- 
ication of amphipod crustaceans: problems in resolut- 
ion. Amphipacifica 1(3): 76-134. 

— — , & N. L. Tzvetkova, 1982. Studies on Dog- 

ielinotidae (Amphipoda, Talitroidea) from the shallow 
waters of the North Pacific region. Expl. Fauna Seas 
1982, 29 (37): 76-94. (In Russian). 

Bulycheva, A. N., 1952. Novye vidy bokoplavov (Amphi- 
poda-Gammaridaea)iz JaponskovoMorei. ILAkad. Nauk 
SSSR. Trud. Zool Inst. 12: 195-250, 39 figs. 

Conlan, K. E., 1983. The amphipod superfamily Corophioidea 
in the northeastern Pacific region. 3. Family isaeidae: 
systematics and distributional ecology. Natl Mus. Nat.Sci 
(Ottawa) Publ. Nat. Sci.: 1-75. 

Coyle, K. O, & G. J. Mueller, 1981. New records of Alask- 
an marine Crustacea. Sarsia 66: 7-18, 5 figs. 

Dang, N. T., 1968. Amphipods of North Vietnam. Zool. 
Zhum. 47: 212-222, 4 figs. 

Gurjanova, E. F., 1951. Bokoplay Moreii SSSR i sopred- 
'elylnik vod (Amphipoda-Gammaridea) Akad. Nauk 
SSSR Opred. po Faune SSSR 41: 1029 pp., 705 figs. 

^ , 1953. Novye dopolnenija k dal' nevost- 

ochnoi faune morskik bvokoplavov. Akad. Naul SSSR. 
Trud. Zool. Inst. 13:21 6-24 1 , 1 9 figs. 

- , 1962. Bokoplavy severnoi chasti Tixogo 


Okeana (Amphipoda-Gammaridea) chasf 1 .Akad. Nauk 
SSSR. Opred. po Faune SSSR 74: 440 pp, 143 figs. 

Hirayama, A., 1985. Taxonomic Studies on the shallow- 
water gammaridean Amphipoda of West Kyushu, Japan 
rv. Publ. Seto Mar. Biol. Lab. 30: 1-53., figs. 124- 161 

Hughes, J.E., 1982. Life history ofthesandy-beach amphipod 
Dogielinotus loquax (Crustacea: Dogielinotidae) from 
the outer coast of Washington, USA. Mar. Biol. 72(2)- 
167-175. 

Ishimaru, S., 1994, A Catalogue of Gammaroidean and In- 
golfiellidean Amphipoda recorded from the vicinity of 
Japan. Rept. Sado Mar. Biol. Sta., Niigata Univ., No. 24: 
29-86. 

Jarrett, N. E., & E. L. Bousfield, 1994a. The amphipod sup- 
erfamily Phoxocephaloidea on the Pacific coast of North 
America. Family Phoxocephahdae. Part I. Metharpiniinae, 
new subfamily. Amphipacifica I (1): 58-140. 

, & E. L. Bousfield, 1994b. The amphipod sup- 
erfamily Phoxocephaloidea on the Pacific coast of North 
America. Family Phoxocephahdae. Part II. Subfamilies 
Pontharpiniinae, Parharpiniinae, Brolginae, Phoxoceph- 
alinae, and Harpiniinae. Systematics and Distributional 
Ecology. Amphipacifica I (2): 71-150. 

Kamihira, Y., 1981. Life history of sand-burrowing amphi- 
podHaustorioidesjaponicus (Crustacea: Dogielinotidae). 
Bull.Fac.Fish.HokkaidoUniv.32(4):338-348. 

Lincoln, R. J., 1979. British Marine Amphipoda. London: 
British Museum (Natural History). 658 pp., 280 figs. 

McLeay, et al. 1992. Acute Test for Sediment Toxicity Us- 
ing Marine or Estuarine amphipods. Environmental Pro- 
tection Series Biological Test Method. Report to Envir- 
onment Canada, MS Report, 1 16 pp., May, 1992. 

Schram, F. R., 1986. Crustacea. Oxford Univ Press, New 
York. 602 pp. 

Sneath, P. H. A., & R. R. Sokal, 1973. Numerical Taxon- 
omy. W. H., Freeman, San Francisco. 573 pp. 

Staude, C. P., 1987. Amphipoda: Suborder Gammaridea. 
pp. 346-391. ip E. Kozloff (ed.) Intertidal Invertebrates 
of the Pacifc Northwest. University Washington Press, 
Seattle. 511 pp. 

Stebbing, T. R. R., 1906. Amphipoda: Gamaridea. Das 
Tierreich. I. Berlin. 806 pp. 

Thomson, R. E., 1981. Oceanography of the British Col- 
umbia coast, Canada, Fish. & Aqu. Sci., Special Publ 
No 56: 1-291. 

Thorsteinson, E. D, 1941. New or Noteworthy Amphipods 
from the North Pacific coast. Univ. Washington, Publ. 
Oceanogr. 4: 50-96, 8 pis. 

Yee, S., M. Van Rikxoort, & D. McLeay, 1992. The effect 
of holding time on Eohaustorius washingtonianus dur- 
ing ten-day sediment bioassays and reference toxicant 
tests. Report to Environment Canada & Intergovern- 
mental Aquatic Toxicity Group. 40 pp.. Appendix. 


AMPHIPACMCA VOL. 11 NO. 1, AUG. 31, 1995 64 


The Canadian Field-Naturalist 

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Francis R. Cook 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


65 


THE AMPHIPOD FAMILY PLEUSTIDAE ON THE PACIFIC COAST OF NORTH AMERICA: PART IH. 
SUBFAMILIES PARAPLEUSTINAE, DACTYLOPLEUSTINAE, AND PLEUSIRINAE. SYSTEMATICS AND 

DISTRIBUTIONAL ECOLOGY. 

by E, L. Bouslield^ & E. A. Hendrycks^ 


ABSTRACT 

The gammaridean amphipod subfamily Parapleustinae Bousfield & Hendrycks, 1994, contains 28 described species 
of which 26 have been recorded from coastal marine regions of the North Pacific Ocean. From shallow coastal shelf waters 
of the both continental coasts are here described and figured the following tax a: Parapleustes americanus, new species; 
P . ishimarui, new species; Chromopleustes lineatus, new genus, new species; Gnathopleustes serratus new genus, 
new species, G. simplex, new species; G. trichodus, new species; G. pachychaetus, new species; Trachypleustes 
vancouverensis, new genus, new species; T. trevori, new species; Micropleustesnautiloides, new genus, new species 
and M, behningiodes, new species. Also proposed for inclusion within the subfamily ar^ Commensipleustes, new genus 
(type species; C. commensalis (Shoemaker, 1952); Incisocalliope J. L. Barnard, 1959 (revived status) (type species; 
/. newportensis Barnard, 1959). This genus contains eight species of which is newly described 
from the Sea of Japan. Also variously redescribed, or treated, are; Gnathopleustes den (J. L. Barnard, 1969b); G. 
pugettensis (Dana, \%5^)\ Incisocalliope newportensis J. L. Barnard, 1959; /. bairdi (Boeck, 1871); Chromopleustes 
oculatus (Holmes, 1908); C. johanseni (Guijanova, 1951); Micropleustes nautilus (J. L. Barnard, 1969b) and M. 
behningi (Guijanova, 1938). Dactylopleustes echinoides, new species (subfamily Dactylopleustinae Bousfield & 
Hendrycks, 1994) is newly described and figured, andPleusirus secorrus J. L. Barnard, 1969b (subfamily Pleusirinae 
Bousfield & Hendrycks, 1994) is redescribed and figured. 

Taxonomically, the seven parapleustin genera were found to be morphologically distinctive, and not very closely 
similar. A modified phenetic cluster analysis indicated that the most southerly, temperate and subtropical genus 
Incisocalliope is phyletically most advanced, and that the mainly N. American cold temperate genus Chromopleustes 
is the most primitive, despite the relatively advanced nature of its mouthparts, and weakly sexually dimorphic gnathopods. 

Biogeographically, of the 26 species of Parapleustinae recorded from the North Pacific region, 16 species (in seven 
genera; occur along the North American coast, nine species (in four genera) along Asiatic shores, and one species in 
the Hawaiian Islands, south central North Pacific. The genera Parapleustes, Chromopleustes, Micropleustes, 
Dactylopleustes andPleusirus are Pan-Pacific, with approximately equal numbers of species on North American and 
Asiatic coasts. However, the generaTrachypleustes, Gnathopleustes and Commensipleustes, containing about a dozen 
species in total, are apparently endemic to the North American Pacific region. The isolated occurrence of Parapleustes 
gracilis (Buchholz, 1874), and Incisocalliope aestuarius (Watling & Maurer, 1973) in different temperature regimes of 
the North Atlantic region, appear anomalous. Although explanations proposed for such disjunct distributions are not 
entirely satisfactory, they underscore the high regional endemicity of subfamily Parpleustinae within the North Pacific 
Basin. 


INTRODUCTION 

Pleustid amphipods form an important assemblage of 
microcarnivorous amphipod crustaceans in the North Pacific 
marine region. Of the 12 recognized subfamilies (Bousfield 
& Hendrycks, 1994), the Parapleustinae, with nearly 30 
described species, is one of the largest and numerically 
dominant groups in shallow-water habitats of both Asiatic 
and North America coasts. The monotypic subfamily 
Pleusirinae is common along the North American coast. 
Species of Dactylopleustinae are commensals on echinoid 
echinoderms, rarely encountered, and the subfamily prob- 
ably more diverse than the three known species would 
indicate. 

Prior to the present investigation, only eight species of 
subfamily Parapleustinae had been recorded from North 
Amer-ican Pacific localites, all of which had been relegated 
to the genus Parapleustes by Barnard & Karman (1991). 

1 Research Associate, Royal Ontario Museum, Toronto, Canada : 

2 Research Assistant, Canadian Museum of Nature, Ottawa, Canac 


Early 19th century records of Dana, Stimpson, Boeck and 
others had been capably summarized by Stebbing (1906). In 
the first half of this century. Holmes (1908) described Ple- 
ustes oculatus from off California. Few other records accrued 
until J. L. Barnard commenced his monumental series of 
studies (1952, 1954, 1956 et sequ.) on amphipod commun- 
ities of the California coast. His paper with Given (1960) 
summarized information on five parapleustins known to that 
date, including Parapleustes newportensis Barnard, 1959, 
that had been described initially as the type species of a new 
genus, Incisocalliope. Shoemaker (1952) had earlier des- 
cribed P. commensalis from the pleopods of a spiny lobster 
off southern California, and later (1964, posthumously) 
added to records of Dana's "Parapleustes pugettensis" from 
Dillon Beach, California. Dana's species name was here 
found to embody several distinct taxa, mostly new to science. 
Barnard (1969b) described Parapleustes den, P. nautilus 
and Pleusirus secorrus from the Central California coast, 

KIP 6P4. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


66 


and the following year (1970) added P. derzhavini makiki 
from the Hawaiian Islands. Very recently, Barnard & 
Karaman (1991) submerged P.johanseni Gurjanova, within 
P. oculatus Holmes, and synonymizedP. bairdi (Boeck) and 
P. newportensis (Barnard) with P. pugettensis (Dana). The 
pragmatic illustrated keys of Barnard ( 1975), Staude (1987), 
and the regional annotated listing of Austin (1985), provide 
useful summaries of existing knowledge and bases on which 
to conduct further studies. 

On the Asiatic Pacific coast, work on parapleustins 
commenced with Gurjanova’s description of Neopleustes 
derzhavini and Pleustes behningi (1938) and Parapleustes 
johanseni (1951). Kudryaschov (1972) provided records of 
P. nautilus (later proven to be a new species). Tzvetkova 
(1975) described the echinoid commensal species Para- 
pleustes echinoicus, later given separate generic status (as 
Dactylopleustes) by Karaman & Barnard (1979). Kudry- 
aschov & Tzvetkova (1975) concluded the Russian contrib- 
ution with a description of Pleusirus secorrus asiaticus. 

Workers from Japan entered the western Pacific para- 
pleustin scene with Irie & Nagata's preliminary regional 
listing (1962) of "Parapleustes oculatus" and "P. pugettensis". 
Ishimaru (1984) contributed most significantly with Para- 
pleustes dilatatus n. sp., P. longimanus, n. sp., and records 
of Parapleustes gracilis Buchholz, P. behningi Gurjanova, 
and P. derzhavini Gurjanova. Soon after, Ishimaru (1985) 
added Pleusirus secorrus to the regional list. Hirayama 
(1988) described Parapleustes filialis, n. sp. and Dactylo- 
pleustes obsolescens, n. sp. Finally, Ishimaru (1994) treated 
the entire pleustid fauna of Japan in his useful regional 
catalogue of gammaridean and ingolfiellidean species. 

The previous studies had revealed a significant new 
fauna of parapleustinids, pleusirins and dactylopleustins in 
the western Pacific and Californian regions. However, 
corresponding faunas of the enormous intervening costal 
areas were virtually unknown. Based on extensive new 
material from the coasts of British Columbia, southeastern 
Alaska, and Washington and Oregon states, the present study 
attempts to fill this large hiatus in systematic knowledge. It 
also attempts to relate these faunas phyletically and bio- 
geographically to faunas of adjacent regions and elsewhere. 

ACKNOWLEDGEMENTS 

The authors are greatly indebted to colleagues and their 
research institutions who provided field assistance, facilities 
and materials that made this study possible. Most of the field 
work was conducted by the senior author (ELB) during the 
period 1955 -1980, station lists for which have previously 
been made available (Bousfield 1958, 1963, 1968;Bousfield 
&Jarrett, 1981; Bousfield & McAllister, 1962). Ship-assisted 
parts of the work were based at the Pacific Biological Station, 
Nanaimo, with the help of the late D. B . (Dan) Quayle; at the 
Pacific Environmental Institute, West Vancouver, with the 
help of C. D. Levings; at the Bamfield Marine Station, with 
the help of A. D. Spencer and colleagues, and at the Friday 
Harbor Laboratories, with the help of C. P. Staude. 


The bulk of the study material is currently maintained by 
the Invertebrate Collections Unit, Canadian Museum of 
Nature (CMN), Ottawa. For the loan of study specimens, the 
authors thank Dr P. Slattery, Moss Landing, CA (Bering Sea 
material); the Los Angeles County Museum, Los Angeles, 
CA (J. L. Barnard material from Southern California), Dr 
Akira Hirayama, Kumamoto, Japan (Japanese material and 
from Russia (formerly USSR), Nina Tzvetkova, and the late 
Eupraxie F. Gurjanova whose extensive publications on the 
far-eastern pleustid fauna have been invaluable reference 
bases for the present study. Helpful commentary on various 
phases of manuscript preparation was provided by Pierre 
Brunei, University of Montreal, Roger Lincoln, British Mus- 
eum, C. P. Staude, Friday Harbor Laboratories, K. E. Con- 
lan, CMN, Ottawa, and Patrick Shaw, Vancouver, B. C. 

The line illustrations were prepared with the most capable 
assistance of Susan Laurie-Bourque, Hull, Quebec (see 
legend for figures, p. 133). Maijorie Bousfield, Montreal, 
provided translations of pertinent Russian literature. 

SYSTEMATICS 

Family PLEUSTID AE 

PARAPLEUSTINAE, Bousfield & Hendrycks, emended 
Parapleustinae Bousfield & Hendrycks, 1994; 41. 

Type genus. Parapleustes Buchholz, 1874 (p. 67). 

Genera. Chromopleustes, new genus (p. 73); Com- 
mensipleustes, new genus (p. 82); Gnathopleustes, new 
genus (p. 82); Incisocalliope J. L. Barnard (p. 95); Trachy- 
pleustes, new genus (p. 105); Micropleustes, nev^ genus (p. 
111 );. 

Removals. Parapleustes assimilis (Sars,1883); P. 
bicuspis (Kroyer, 1838); P. monocuspis Sars, 1895; P. gag- 
arae Gurjanova, 1972; P. major Bulycheva, 1952, P. bi- 
cuspoides NugatSi, 1965; P. sinuipalmaDunbar, 1947, P. tri- 
anguloculatusBulycheva, 1952; P. tricuspislshimaru, 1984, 
to genera within subfamily Neopleustinae (Bousfield & 
Hendrycks, 1994, and in prep.). 

Diagnosis. Body generally small to medium, smooth 
above, not mucronate on pleon; external surface pattern 
often colourful or disruptive. Head, rostrum short, little or 
not exceeding rounded lateral head lobe. Eyes variable in 
size and form, usually medium large, subrotund. Antennae 
usually elongate; antenna 1 the longer, occasionally short, 
peduncular segments often shortened. Accessory flagellum 
minute. 

Mouthparts generally strongly modified. Upper lip 
distinctly notched, lobes variously asymmetrical. Lower lip 
broad, squat, outer lobes oblique. Mandible, molar small, 
weak, thumblike, apex pilose, triturating surface lacking or 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


67 


vestigial; blades generally numerous, often strongly modified: 
chisel-shaped, cusplike, or molarized in form; left lacinia 
wide, multidentate, cutting edge straight; right lacinia lack- 
ing; incisor multidentate, third (distal) tooth largest; palp 
segment 3 not shorter than 2, with basal “A” seta (of Cole, 
1980). Maxilla 1, inner plate with single apical seta; outer 
plate with 9 (rarely 15-18) apical spine teeth; palp occasionally 
broadened, with distal facial setae, apices spinose; segment 
1 often with lateral ("shoulder") seta(e). Maxilla 2 ordinary, 
inner palate with stout inner marginal plumose seta(e). 
Maxilliped; palp strong, segment 2 usually longest, 3 lacking 
distinct distal process; outer plate narrow (vertical margins 
subparallel), sparsely setose and/or spinose; inner plate 
short, apex with “button” spines, inner margin with few setae 
and/or spines. 

Coxal plates large, deep, broad; coxa 1 generally broad- 
ening distally and rounded below; hind comers cuspate. 
Gnathopods various; weak to medium strongly developed; 
gnathopod 2 slightly larger, differing slightly in form, and 
occasionally sexually dimorphic. Gnathopod 1, basis, margins 
variously setose; meral cusp weak; propod, palm usually 
oblique, convex, with median tooth. 

Peraeopods 3 & 4 ordinary, normally spinose, dactyls 
short to medium. Peraeopods 5-7 homopodous; coxae 
medium deep, hind margins rounded, laterally smooth; 
segment 4 longer than 5 which it variously overhangs behind. 

Pleon plates 2-3, hind comers acuminate, not produced. 
Pleopods medium strong, ordinary. Uropods 1 & 2 ordinary; 
peduncle of uropod 1 with prominent distolateral spine; rami 
elongate, outer shorter, margins and apex strongly spin-ose. 
Uropod 3, inner ramus markedly the longer, margins spinose. 

Telson elongate, narrowing distally, keeled proximally; 
apex rounded; penicillate setae medio-distal. 

Coxal gills variable, smaller and saclike anteriorly, 
larger, platelike posteriorly. Brood plates large, broad. 

Distributional ecology. The subfamily is essentially 
endemic to eulittoral shelf habitats of the North Pacific 
region. However, three species occur in isolation elsewhere, 
viz., the northeastern North Atlantic, the western North 
Atlantic, and the Hawaiian Islands of the central North 
Pacific (seep. 131). 

Taxonomic commentary. The Parapleustinae is closely 
allied to subfamily Neopleustinae (Bousfield & Hendrycks, 
1994). The latter differs, however, in having a well-developed 
keeled rostmm, dorsal body processes, a short, nearly centrally 
keeled telson, large mandibular palp, and a distally oblique 
and processiferous maxillipedal palp segment 3. Also, 
component members of the Neopleustinae occur in deep cold 
waters of the Arctic, North Atlantic and North Pacific 
regions; none is intertidal. 

Numerical taxonomic analysis of the Parapleustinae 
reveals a complex of 7 generic-level subgroups (Fig. 43, p. 
127), the species of which are treated systematically below. 


Parapleustes Buchholz 

Parapleustes Buchholz, 1874: 337.— Stebbing 1906: 320.— 
Gurjanova, 1951: 648 (partim).— Barnard 1969a: 425 
(partim). — Barnard & Karaman, 1991: 649 (part). 

Type species, Parapleustes gracilis Buchholz, 1874. 

Species composition (North Pacific). Parapleustes 
ishimarui (= P. gracilis Ishimaru, 1984) (p. 70); and P. 
americanus, new species (p. 71). 

Diagnosis. Body small, smooth above. Head, rostrum 
very short; anterior head lobe subacute; inferior antennal 
sinus broadly incised. Eye medium, elliptical to roundish. 
Antennae slender, medium long, weakly setose. Antenna 1 
typically the longer; peduncle 3 short; peduncle 1, distal 
process weak; accessory flagellum minute. 

Mouthparts modified. Upper lip shallowly notched, 
lobes asymmetrical. Lower lip medium wide, squat; outer 
lobes thick, rounded, oblique. Mandible: molar reduced to 
a blunt setulose knob; incisor irregularly toothed, distal teeth 
smaller; left lacinia 8-10 dentate; blades 5-12 in row, stout, 
weakly molarized; palp slender, segment 3 with few (3-5), 
posterior marginal “D” spines; maxilla 1, outer plate with 9 
mainly tall apical spines; palp not broadened, with -4 apical 
spines and several oblique subapical (facial) setae. Maxilla 
2, inner plate little broadened, with marginal plumose seta. 
Maxilliped, palp strong, dactyl strong, segment 3 lacking 
distal process; segment 2 largest; outer plate short, little or 
not longer than inner, 1(2) apical spines; inner plate with few 
apical button spines and few marginal setae. 

Coxal plates wide, deeper than respective body plates; 
lower margins straight, hind notch(es) distinct; coxa 1 little 
smaller than 2, slightly expanded distally. 

Gnathopods medium large, closely subequal, little or 
not sexually dimorphic; propods broadening distally, palms 
smoothly convex, usually with central median tooth, postero- 
distal angle with 1-2 clusters of spines not extending onto 
palm; hind margin smooth, about equal in length to palm; 
carpus usually short, hind lobe deep; postero-distal process 
of merus acutely produced; bases slender, antero-marginal 
setae distally restricted. 

Peraeopods 3-7 slender, weakly spinose; segment 5 and 
dactyls slender, relatively long. Peraeopods 3-4, margins of 
segments 4-6 weakly spinose, lacking special setae. 
Peraeopods 5-7 regularly homopodous, bases broad, convex 
behind. 

Pleon plates broad, deep, smooth behind, hind comers 
weakly acuminate. Pleopods strong, not sexually dimorphic. 
Urosome short; urosome 2 not occluded dorsally. Uropods 
1 & 2 rami slender, tips spinose, usually extending beyond 
uropod 3. Uropod 1, peduncle with distinct latero-distal 
spine; rarm subequal in length. Uropod 2, inner ramus the 
longer. Uropod 3, inner ramus markedly the longer. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


68 


KEY TO KNOWN GENERA OF SUBFAMILY PARAPLEUSTINAE 

1. Gnathopods 1 & 2, palm of propod with median tooth present, variously developed; gnathopod propod, 

length of palm about equal to (or longer than) posterior margin; gnathopod propods, hind margin lack- 
ing setae (except some Incisocalliope)’, gnathopod 2, carpus always relatively short, anterior margin 
<1/2 length of propod 3. 

— Gnathopods 1 & 2, propodal palm, median tooth lacking or very reduced; gnathopod propod, length of 
palm short, usually much less than posterior margin (except in some Micropleustes)\ propod, hind mar- 
gin with 1 - 4 setae or setal groups; gnathopod 2, carpus usually elongate, anterior margin about equal 
in length to propod (except some Micropleustes) 2. 

2. Antennae slender, flagella elongate, antenna 1 usually markedly the longer; peraeopods 5-7, segment 4 
postero-distally overhanging segment 5 by less than 1/4 length of segment 5; coxal plates 2 - 4 not ex- 
ceptionally large and/or deep, distal portions of respective bases exposed below, hind cusps of coxae 

2 & 3 single Chromopleustes (p. 73) 

— Antennae short, stout, subequal, flagella little (or not) longer than respective peduncles; peraeopods 5 - 

7, segment 4 overhanging segment 5 postero-distally by nearly half length of segment 5; coxae 2 - 4 
large and deep, totally masking respective bases, hind comers with 2-5 small cusps (rarely single) .... 
Micropleustes (p. Ill) 

3. Antennae short, flagellum; of A1 little longer than peduncle, of A2 shorter than peduncle; gnathopods 1 

& 2, carpus very short, length less than 1/4 that of propod, hind lobe small, narrow; pleon plate 3, hind 
comer with small hook Parapleustes (p. 67) 

— Antennae normally elongate, flagellum distinctly longer than respective peduncle; gnathopds, dorsal 
margin of carpus more than one-fourth length of propod, hind lobe about half as wide as its dorsal mar- 
gin; pleon plate 3, hind comer acuminate, not mucronate 4. 

4. Peraeopods 5-7, segment 6 broadened distally, anterior margin with stout spines, forming (with dactyl) 

a grasping organ; maxilliped, outer plate shorter than inner plate; coxa 1 not noticeably broadening 
distally, hind margin lacking proximal short spine(s) Commensipleustes (p. 82) 

— Peraeopods 5-7, segment 6 normally slender and spinose; maxilliped, outer plate slightly longer than 
inner plate; coxa 1 broadening distally, hind margin with proximal spine(s) 5. 

5. Gnathopods large, strongly subchelate, variously sexually dimorphic; basis, anterior marginal setae 

confined to distal angle; antenna 2, peduncular segments not shortened, surfaces armed variously with 
clusters of short setae Gnathopleustes (p. 82) 

— Gnathopods medium subchelate, propod and carpus combined shorter than depth of coxa, not sexually 
dimorphic; basis, anterior margin often setose throughout; antenna 2, peduncular segments 4 & 5 
shortened and/or bare of surface setal groups 6. 

6. Antenna 1, peduncular segment 2 short, less than half length of segment 1; mandible, palp segment 2 

weakly setose (6-7 setae); left lacinia 10-12 dentate; maxilliped, palp segment 3 lined medio-distally 
with short spines Incisocalliope (p. 95) 

— Antenna 1, peduncular segment 2 not shortened, length greater than half that of segment 1; mandible, 
palp segment 2 with numerous (10-15) medial setae; left lacinia 7-9 dentate; maxilliped, palp segment 

3 lacking distal short spines Trachypleustes (p. 105) 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


69 



FIG. 1. Parapleustes gracilis Buchholz. Female (2.5 mm). Norwegian Sea. (after Sars, 1895). 


Telson medium long, narrowing, subacute; dorsal 
penicillate setae slightly distad (of middle). Coxal gills sac- 
like, medium, unequal, smallest anteriorly. 

Taxonomic commentary. The following species are 
TQmoytdfromParapleustes, sens. str.\ P. assimilis Sars and 
P. tricarinatus lsYmR^nx-{\.oNeopleustesy,andP. commens- 
alis Shoemaker (to Commensipleustes), for the following 
combination of reasons: lack of a disto-lateral spine on the 
peduncle of uropod 1 ; the peraeopods are too long, or stout, 
dactyls too short; gnathopod propods are too slender, and/or 
the posterior margin is too strongly setose; the palmar tooth 
is lacking; the carpus is too long, shallow; the mouthparts are 
significantly different, especially in the mandibular blades; 
and the pleon is dorsally carinate. 

Within Parapleustes proper, the markedly smooth 
propods and narrow carpal lobes of the gnathopods might 
suggest a closer relationship with the genera Pleustes and 
Pleusymtes. 

Distributional commentary. The genus Parapleustes 
(sens, str.) is essentially arctic-subarctic in present distribut- 
ion, dipping southward variably, and mainly subtidally in the 
North Pacific and northern North Atlantic regions. Para- 
pleustes gracilis is not typical of the subfamily but became 
the type species because it is the only member occurring in 
the North Atlantic region where amphipod taxonomy began. 


Parapleustes gracilis Buchholz 
(Fig. 1) 

Parapleustes gracilis Buchholz, 1874; 337, fig. 1.— Steb- 
bing, 1906: 320.— Gurjanova, 1951: 648, fig. 444.— Bar- 
nard & Karaman, 1991: 650. 

non Parapleustes gracilis Ishimaru, 1984. — Hirayama, 
1988? 

Paramphithoe brevicomis G. O. Sars, 1895: 353, pi 124. 2. 

Diagnosis. Female (2.5 mm); Head, eye medium 
roundish, black. Antenna 1, peduncular segment 2 short, 
length -1/2 segment 1; flagellum 13-segmented. Antenna 
2, peduncular segments 4 & 5 slender, subequal; flagellum 
8-segmented. 

Mouthparts not described (notin Sars 1895, norStebbing, 
1906) but probably similar to those ofP. americanus (p.71). 

Coxae 1-3 deep, medium broad, lower margins weakly 
convex, hind comers each with single cusp. Gnathopod 1, 
basis with weak antero-distal setal cluster; mems with acute 
postero-distal process; carpus short, hind lobe narrow, deep; 
propod distinctly expanding distally, inner face smooth; 
palmar margin oblique, convex, postero-distal angle with 
spine groups on either side of distinct dactyl-tip depression. 
Gnathopod 2 closely similar in size and form; basis, antero- 
distal margin with several setae. 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


70 



Peraeopods 3 & 4, bases with several antero-distal 
setae; segments 4-6 slender, elongate (especially segment 
6); segments 4 & 5 subequal in length; marginal setae sparse; 
dactyl curved, elongate, length >1/2 segment 6. Peraeopods 
5-7 slender, bases medium broad, postero-distal lobes shallow; 
segments 4 & 5 subequal; segmentb elongate; dactyl elongate, 
length > 1/2 segment 6. 

Pleon plate 3 , hind comer weakly acuminate, not hooked . 
Urosome 2 with free dorsal margin. Uropods 1-2 slender, 
peduncle and rami weakly spinose. Uropod 3, outer ramus 
2/3 length of slender inner ramus . Telson medium, length 
~1.5X basal width, apex subacute. 


fauna. Of the 21 species of Parapleustes listed by Barnard 
& Karaman, most are members of subfamily Parapleustinae, 
but only P. gracilis (= P. brevicomis Buchholz?) is retained 
in the genus Parapleustes. All others are removed to other 
genera, and in some cases, other subfamilies. It has been 
found advisable to restore to the original position a number 
of transfers, and a number of synonymies, by others. Thus, 
Micropleustes nautilus is removed from the synonomy of M. 
behningi, and restored to full species recognition, and the 
genus Incisocalliope J. L. Barnard, 1959, is removed from 
the synonomy of Parapleustes Buchholz and restored to its 
original full generic position. 


Distributional commentary. This species is endemic 
to arctic and arctic-boreal, North Atlantic waters. It has not 
been recorded authentically from the North Pacific region. 
As the type species of the genus, this North Atlantic form is 
included here for comparative purposes with North Pacific 
material previously ascribed to the name Parapleustes gracilis 
(above). 

Taxonomic commentary. Parapleustes gracilis is the 
type of a small group of species here restricted to a few 
members of the North Atlantic and North Pacific pleustid 


Parapleustes ishimarui, new species 
(Fig. 2) 

Parapleustes gracilis Ishimaru, 1984; 432, figs. 21-24. — 
Ishimaru, 1994: 54. 

Diagnosis. Female (2.4 mm): Head, eyes small, round, 
black. Antennae short. Antenna 1, peduncular segment 2 
medium, length > 2/3 peduncular segment; accessory 
flagellum, apex rounded, with 1 plumose and 2 simple setae; 
flagellum 9-10 segmented. Antenna 2, peduncular segment 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


71 


KEY TO KNOWN SPECIES OF PARAPLEUSTES (SENS. STR.) 

. 1 , peduncle 2 short; peraeopod 7, basis, posterior margin nearly straight; uropods 1 & 2, rami shorter 

-A~T ^ f P- (Buchholz)(p. 69) 

enna 1, peduncle 2 normal; peraeopod 7, basts, posterior margin strongly convex; uropods 1 & 2 

inner ramus about equal m length to peduncle; peraeopods 1 & 2, dactyls shorter (<l/2 propod) . . , . ’ 2. 


2 Peraeopod 7, basis finely crenulate; pleon plate 3, hind comer forming small hook or mucrona; eye 

large, ovme; naaxtlhped outer plate short antericanus. n. sp. (p. 73) 

Peraeopod 7, basts with few (8) large posterior notches along posterior margin; pleon plate 3, hind 
comer blunt-acuminate; eye small, round; maxilliped, outer plate normal, equal in length to inner plate . 
P. ishimarui, n. sp (p. 71) 


5 slender, slightly shorter than segment 4; flagellum short, 6- 
segmented. 

Upper lip conical, apex shallowly incised, lobes slightly 
asymmetrical. Lower lip, inner lobes deep, not broad; outer 
lobes shallowly oblique. Mandible, molarprominent. slightly 
upturned apically; spine row with 6-7 short blades; cutting 
edge (left) with 3-4 large teeth proximally and 4 small 
denticles distally; palp segment 3, basal “A” setae short; 
postero-distal margin with 4 pectinate “D” spines; left lacinia 
10-dentate. Maxilla 1, inner plate with single short seta; 
palp, apex sharply rounded, with 4 slender spines. Maxilla 
2, inner plate broad, length nearly equal to outer plate, inner 
margin with short proximal seta. Maxilliped, inner plate 
broad, with 3 apical marginal “button” spines; outer plate 
medium, taller than inner plate, apex blunt, with 2 unequal 
slender spines; palp segment 3 slender, dactyl slender almost 
straight. 

Coxae 1-3 lower margins get^y convex, hind comers 
with single cusp. Coxa 4 hind marginal process rounded. 
Gnathopod 1, basis with weak antero-distal setae; merus 
with cusp; carpus short, hind lobe narrow, deep; propod 
expanding distally with weak inferior facial setae, palmar 
margin longer than convex posterior margin, postero-distal 
angle with weak distal and strong proximal spine groups 
adjacent to dactyl-tip depression. Gnathopod 2 closely 
similar in form but propod slightly smaller, and basis lacking 
antero-distal setal group. 

Peraeopods 3 & 4 regular, slender, segment 5 relatively 
short (<segment 4), margins weakly spinose; dactyl short (~ 
1/3 segment 6). Peraeopods 5-7 subsimilar, increasing 
slightly in size posteriorly; segment 4 and dactyl relatively 
short. Peraeopod 7, basis more broadly expanded, hind 
margin weakly crenulate. 

Pleon plate 3, hind comer subquadrate. Uropods 1 & 2 
relatively short, margins weakly spinose, outer ramus 
distinctly the shorter. Uropod 3, outer ramus short, length 
~60% stout inner ramus. Telson subrectangular, narrowing 
slightly distally, apex broadly rounded. 

Type material. Ishimaru (1984): Female "a" (3.4 mm) 
Holotype; intertidal, Ohzuchi, Japan. Zoological Museum 
collections. Faculty of Science, Hokkaido University. 

Distribudon. Known from a single intertidal station, at 
Ohzuchi, Iwata Prefecture, northeastern Japan. 


Etymology. The species is named in named in honour 
of Dr Shin-ishi Ishimam who has contributed very signifi- 
cantly to knowledge of the marine amphipod fauna of Japan 
and adja-cent regions. 

Taxonomic commentary. Parapleustes ishimarui 
appears most closely related to P. americanus but differs in 
characters provided in the key (above). 

Parapleustes americanus, new species 
(Fig. 3) 

Parapleustes pacifica (?) Austin, 1985: 592.— Barnard & 
Karaman, 1991: 650 (part). 

Material examined; 

ALASKA. 

Bering Sea: N. E. of St. Lawrence I., P. Slattery, Dive 2, July 
9, 1980 - 2 females. Punuk I., 5 m dive, gravel, P. Slattery 
coll., July 6, 1983 - 1 1 specimens, including females, males 
and im. 

SE Alaska, ELB Stn. A48, Icy Strait, sand and gravel at LW 
level, June 17, 1948 - 5 females. 

BRITISH COLUMBIA. 

North-central coast: ELB Stn. H25 (Cox Pt. Inlet), 6 m 
dredge, muddy sand, July 18, 1964 -7 im; H48 (Goose I.), 

8 m dredge, sand, kelp, Aug. 5, 1964 -2 females. Paratypes 
(slide mounts), CMN Cat. no. NMCC 1955-0082. Swanson 
Bay, C. Levings Stn. 51B-031, Apr. 4, 1973 - 1 im. 

Vancouver I., north end: ELB Stn. V20 ( Brown Bay), coarse 
sand at LW, June 22, 1959 - 1 female ov, Holotype (slide 
mount), CMN Cat. no. NMCC 1995-0081. 

Vancouverl., Southend: ELB Stns.,July5, 1976: B 16 (off 
Bordelais L), 44-50 m dredge, sand and gravel- 4 females 
ov.; B20 (off Long Beach, Trevor Channel), 30 m dredge, 
gravel - 2 females ov. 

Diagnosis. Female ov (3.0 mm): Head, eye medium 
large, nearly round, black. Antenna 1, peduncular segment 
2 long, length nearly equal to segment 1; flagellum 15- 
segmented. Antenna 2, peduncular segments 3 & 4 slender, 
subequal; flagellum 10-segmented. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 



73 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 

either side of pronounced dactyl-tip depression; dactyl 
slender, with short terminal nail. Gnathopod 2 closely 
similar, propod slightly smaller. 

Peraeopods 3 & 4 slender, segment 5 long (~ segment 4) 
marginal spines slender; dactyls medium long. Peraeopods 
5-7 slightly increasing in size posteriorly; bases medium 
broad, postero-distal lobes medium deep, hind margins gently 
convex; distal segments slender, segment 5 long (~ segment 
4); dactyls medium. 

Pleon plate 3, hind comer with small hook. Uropods 
slender, spinose. Uropod 1, outer ramus slightly the shorter. 
Uropod2, outer ramus distinctly the shorter. Uropod 3, outer 
ramus short, length -60% slender inner ramus having 5=4- 
5 pairs of marginal spines. Telson narrowing gradually to 
subacute apex. 

Distribution. From the Bering Sea, and southeastern 
Alaska to southern British Columbia, subtidally to depths of 
50 m at southern locations, mainly on coarse sand and gravel 
bottoms. 

Etymology. The species name alludes to its distribution 
along the American coast of the North Pacific Ocean. 

Taxonomic commentary. In most character states, 
including the gnathopod propods and the unshortened segment 

5 of peraeopods 3 & 4, Parapleustes americanus is similar 
to Ae type species, P. gracilis, from the North Atlantic 
region. These two species had been synonomized by Barnard 

6 Karaman (loc. cit.). However, in Parapleustes americanus, 
the hind cusps of coxae 1-3 are more pronounced, urosome 
2 is nearly occluded dorsally and, in uropod 3, the inner 
ramus is relatively short. 

Some morphological differences have been noted 
between material from the Bering Sea and from southern 
parts of its range in British Columbia. These are here 
considered regional variations, not of species significance. 

Chromopleustes, new genus 

Parapleustes Stebbing 1906: 312 (part).— Gurjanova, 1951: 
648(part).— Barnard 1969a: 425 (part).— Barnard & Karaman, 
1991: 649 (part). 

Parapleustinae: oculatus group, Bousfield & Hendrycks 
1994:42. 

Type species. Parapleustes oculatus Holmes, 1908. 

Species composition. Chromopleustes johanseni, Gurj- 
anova, 1951; C. lineatus, new species (p. 78). 

Etymology, a combining form of the Greek ^^kromos"' 
referring to the remarkably disruptively banded and striped 
external body colouration, and the generic name “Pleustes". 

Diagnosis. Body smooth above. Head, rostrum very 
short; inferior antennal sinus short, nearly right-angled. 


Eyes large, nearly round. Antennae well-developed, slender, 
very weakly setose and/or spinose; flagella elongate. An- 
tenna 2 distinctly the shorter; accessory flagellum extremely 
minute or lacking. 

Mouthparts strongly modified. Upper lip deeply 
notched, lobes markedly asymmetrical. Lower lip very 
wide, deep, outer lobes slender, rounded very oblique. 
Mandible, left incisor with numerous (>15), right incisor 
with 9-12, dentations or serrations; left lacinia multicuspate 
(>20); blades tall, slender, numerous (10-15), some with 
basal “satellite” setae; palp segments relatively short, segment 
2 medially sparsely setose. Maxilla 1, apical spines of 
outer plates numerous (13-17), slender tall; inner plate with 
single minute apical seta; palp distally widened, with 6-8 
apical spines and several closely subapical setae. Maxilla 2, 
inner plate not broadened, inner marginal plumose setae 
slender. Maxilliped, segment 3 (outer plate segment) 
strikingly enlarged, much longer and larger than palp segment 
1; segments 2 & 3 short, dactyl strong; inner plate with 2-3 
stout inner marginal setae. 

Coxal plates medium, little (or not) deeper than corre- 
sponding body plates; coxa 1 not broadened or bent distally; 
postero-distal notch single, minute. Gnathopods small to 
medium strong, distinctly sexually dimorphic; propod and 
carpus elongate (especially in female), shorter, broader and 
stouter in male; palm of propod much shorter than posterior 
margin, straight, oblique, lined with short setae, lacking 
median tooth; carpal lobe shallow, medium to broad. 
Gnathopod 1, basis with proximo-posterior “hump”. 

Peraeopods 3-7 stout, medium long, weakly spinose, 
segment 5 strong; dactyls short, strong. Peraeopods 3 & 4, 
margins weakly spinose, lacking special setae. Peraeopods 
5-7 regularly homopodous, bases somewhat narrowed be- 
hind. 

Pleon side plates very broad, medium deep, hind corners 
acuminate but not produced. Pleopods normal, strong, not 
sexually dimorphic. Urosome short, segment 2 not occluded 
dorsally. Uropods regularly spinose; rami of uropods 1 & 2 
distinctly longer than respective peduncles; outer ramus 
slightly the shorter. Uropod 3, rami much longer (3X) than 
peduncle, outer ramus distinctly the shorter. Telson med- 
ium-long, rounding apically. Coxal gills large, platelike. 

Taxonomic commentary. Within the subfamily 
Parapleustinae, the genus Chromopleustes appears to be 
closest morphologically to the genus Incisocalliope, on the 
apomorphic side, and to Gnathopleustes on theplesiomorphic 
side. It is distinguished from the latter, however, rather 
superficially by the more slender antennae; longer, less 
spinose legs with shorter dactyls; more elongate uropods, 
and more striking, disruptive body colouration. In detailed 
characterization, itis most distinct (unique) in the form of the 
mouthparts, with specialized proliferation of pectinate spines, 
blade spines, and multi-dentate incisors and lacinia mobilis. 

To date, members of the genus have not been recorded 
outside the North Pacific coastal marine region, on both 
Asiatic and N. American coasts. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


74 


KEY TO KNOWN SPECIES OF CHROMOPLEUSTES 

1 . Eye small, remote from anterior head margin; antenna 2, flagellum <30-segmented; uropod 3, inner 

ramus with few (4-5) pairs of marginal spines; maxilliped, palp segment 1 longer than 2; Asiatic Pac- 
ific C. johanseni (p. 77) 

— Eyes large, near anterior head margin; antenna 2, flagellum >30-segmented; uropod 3, inner ramus with 
8-10 pairs of marginal spines; maxilliped, palp segment 1 shorter than 2; North American Pacific . . 2. 

2. Gnathopod 2, propod slender (both sexes), length >2X depth; telson elongate, length >2X width; mand- 

ible, left lacinia with about ~40 marginal teeth; maxilliped, inner plate with 3 inner marginal setae; 
telson elongate, length >2X width C. oculatus (p. 74) 

— Gnathopod 2, propod stout (both sexes), length <2X depth; telson short, length -1.5 X width; mandible 
left lacinia with about 20 marginal teeth; maxilliped, inner margin with stout single blade adjacent to 
facial seta; telson short, length -1.5 X width C. lineatus (p. 78) 


Chromopleustes oculatus (Holmes) 

(Fig. 4, 5, 6, 7) 

Neopleuste^ oculatus Holmes, 1908: 531, figs. 36, 37. 
Parapleustes oculatus Barnard & Given, 1960:1. — Barnard, 
1969b: 198 (key).— Bousfield, 1985: 31, fig. 1.— Staude, 
1987: 379.— Barnard & Karaman, 1991: 650. 

Material examined: Nearly 60 specimens in 15 lots 
ALASKA, (numbers of specimens in parentheses): 

Bering Sea: Amchitka I., Aleutians Ids., C. E. O’ Clair Sta. 
IA-2, Oct. 23, 1972 - I im. 

Southeastern Alaska, ELB Stns, 1961 : A3(70); A6(2); A1 8(2); 
A57(l); A168 (8); A174 (13); A175 (31); Stn. A8 (Tongass 
Narrows, opposite Ketchikan), rock and sand at LW, June 3, 
1961 - 1 male (slide mount), (fig. ’d); female ov. (slide 
mount),(fig’d specimen), + 15 male, female specimens. 
ELB Stn. S19B1 (Kameno Pt., near Sitka), July, 1980 -1 
male, 2 im. 

K. E. Conlan Stns., 1989: Torch Bay, 4.6-13.7 m, June 18 
- male, female; Baranof I., Whale Bay, 4.5 - 6 m, June 21 - 
1 male; Bocade Quadra, 30.5 m dredge, June 27 - 3 females; 
Frederick Sound, Brothers I., 5-6 m., P. Slattery coll.. Mar. 
24, 1988 - 8 males, females. 

BRITISH COLUMBIA. 

Queen Charlotte Island, ELB Stns, 1957 : N2a (Parry Passage) 
22 males, females; W8 (2); W15b(2). Naden Harbour, 9 m 
dredge. Sept 16, 1955 -1 female. 

North-central coast: ELB Stns, 1964: H3 (40); H5 (50); 
H7(6); H12(14); H29 (15); H33(30); H50 (60); H53 (16); 
H57 (2); H65 (7). 

South-central coast: Sutton I., Sechelt Narrows, 15 m dive, 
Neil McDaniel coll., July , 1978 - 1 male, 1 female, 7 im. 
Vancouver I., north end: ELB Stns., 1959: 03 (15); 05 
(9)07b (15); V20 (Brown Bay) (9); V5 (Nigei I.) (2). 
Vancouver I., south end: ELB Stns. 1955: FI (1);F2 (1); F4 
(3); P4 (9); P7 (2); ELB Stns., 1976: B4 (1); B5 (2); B8 (5); 
B21b(l). 

CALIFORNIA: 

Off Del Mar, 20 m, R. Rosenthal coll., June, 1969 - 6 im. 


Diagnosis. Male (8. 2 mm): Head, eye large, broadly ovate, 
black. Antenna 1, flagellum with -60 small segments; 
accessory flagellum minute. Antenna 2. peduncle 5 distinctly 
longer than segment 4; flagellum with -45 small segments. 

Upper lip, median notch V-shaped, half depth of labrum. 
Lower lip, inner lobes very broad. Mandible, spine row with 
14-15 slender blades; incisor cutting edge nearly straight, 
with 25-1- teeth, strongest proximally; left lacinia, cutting 
edge slightly concave, with -50 fine teeth; palp segment 3 
with 12 pectinate inner marginal and 3 long terminal setae. 
Maxilla 1, inner plate with single short apical setae; outer 
plate with 12-13 slender apical spines; palp segment 2 
slightly widening distally, with 8-9 apical short spines. 
Maxilla 2, outer plate not wider than inner. Maxilliped , inner 
plate medium, with 3 ordinary inner marginal setae and 5 
small apical denticles; outer plate medium, apex obliquely 
truncated; palp segment 1 shorter than 2. 

Coxae 1-3 relatively narrow, lower hind comer of each 
with minute cusp. Gnathopod 1, hind margin of basis with 
distinct proximal “hump”; carpus short, slightly longer than 
deep; propod slender, longer than deep; palm margin oblique, 
convex, merging imperceptibly with hind margin, postero- 
distal angle with 3+1 groups of short spines. Gnathopod 2, 
carpus short, little longer than deep; propod slender, length 
> 2X depth; palmar margin very oblique, merging with hind 
margin, postero-distal angle with 4 groups of spines and 2 
singly inserted spines. 

Peraeopods 3 & 4 slender; segment 6 with 8- 1 0 posterior 
margin spine groups; dactyls very short, little curved. 
Peraeopods 5-7 closely homopodous in form and size; bases 
not strongly broadened, lower hind lobes shallow; dactyls 
very short. 

Pleon plate 3, hind comer weakly acuminate. Uropods 
1 -3 relatively long, inner ramus > peduncle, margins strongly 
spinose. Uropod 3, inner ramus > 2.5 X peduncle, margins 
with 10-12 serial spines. Telson linguiform, length ~2X 
width, apex rounded. 

Distribution. The species ranges from the Bering Sea 
and southeastern Alaska, south through British Columbia, to 
California, commonly from LW level to depths of 20 m, in 
a variety of habitats, associated with Ulva and bryozoans. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


75 




MXPD 


FIG. 4.Chromopleustesoculatus (Holmes, 1908). Female (11.0 mm). Monterey Bay, California. 
(modified from Holmes, 1908) 



FIG. 5, Chromopleustes sp. 1. (Barnard & Given, 

(after Barnard 


1960). Female (6. 5 mm). Santa Monica Bay, 70 m. 
& Given, 1960) 


Taxonomic commentary. The present female speci- 

mens compare closely with the 11.0 mm female illustrated 
by Holmes (1908) from Monterey Bay (Fig. 4). However, 
they differ from the small mature female illustrated by 
Barnard and Given (loc. cit.) from Santa Monica Bay, south 
of Point Conception, California (Fig. 5). The latter has 
relatively short antennal flagella, larger and broader coxal 


plates 1 -4, broader bases of peraeopods 5-7, relatively weakly 

spinose uropodrami, relatively short telson, and much longer 
inner plate of the maxilliped. In order to clarify its taxonomic 
status, re-examination of the Santa Monica Bay material 
would seem desirable. 

Chrompleustes oculatus displays a disruptive “saddle 

back” colour pattern, with dark vertical stripe and bright yel- 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 76 



FIG. 6. Chromopkustes oculatus (Holmes) Male (8.2 mm); female ov (11.0 mm). Tongass Chan., Alaska 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


77 



FIG. 7. Chromopleustes oculatus (Holmes). Male ov (8.2 mm). Tongass Channel, Alaska. 


low spot on coxa 4 (see Bousfield, 1985, fig. 1), that is one 

of the most striking of all subhttoral North Pacific amphipods . 
The "saddle back" spot is wide, extending fully over the dor- 
sum of peraeon segments 5 & 6, but only over segment 5 and 
half of segment 6 in C lineatus. In C. oculatus, moreover, 
there are 3 dorso-lateral body stripes on each side, vs. 4-5 in 
C. lineatus, and coxal plates 1-3 are white, vs. brownish and 
vertically striped in C. lineatus (p. 81). 

As noted elsewhere (Bousfield & Hendrycks, 1994), 
such may be a form of warning colouration, indicating the 
presence of terpenes or similar body chemicals that are 
distatefiil to fishes and other potential predators. 


Chromopleustes johanseni (Guijanova) 

(Fig. 8) 

Parapleustes johanseni Guijanova, 1951: 550, fig. 446. 

Parapleustes oculatus Barnard & Karaman, 1991: 650. 

Ishimaru, 1994: 54 

Diagnosis, (after Gurjanova, 1951): Female (7.0 mm). 
Head, eyes relatively small, rounded, brownish, remote from 
the anterior margin by an eye width. Antenna 1 slightly 
Shorter than antenna 2; flagellum 21-segmented. Antenna 2, 
flagellum 26-segmented. 


AMPHIPACIFICA VOL 11 NO. 1. AUG. 31, 1995 


78 



FIG. 8. Chromopleustes johanseni (Gurjanova). Female (7.0 mm). Bering Sea. (after Gurjanova, 1951). 


Mandible, spine row with about 20 slender blades; right 

incisor, cutting edge with 12 teeth, largest proximally; palp 
segment 3 with 6-8 pectinate “D” spines. Maxilla 1, inner 
plate narrowly lobate, lacking apical seta; outer plate with 9 
apical spines; palp segment 2 inner margin bulging inward, 
apex with 4 stout spines. Maxilliped, inner plate very short, 
apex setose; outer plate short, apex obliquely truncate; palp 
segments 1 and 3 longer than 2 . 

Gnathopods slender. Gnathopod 1, basis stout, heavy, 
posterior margin with strong proximal “hump”, anterior 
margin richly setose; carpus large, longer than deep; propod 
more slender and a little longer than carpus, length ~2X 
depth, palm short, convex, oblique, postero-distal angle with 
few spines. Gnathopod 2, carpus elongate, length > 2X 
depth, posterior lobe shallow; propod more slender , slightly 
shorter than carpus, palm convex and more oblique than in 
gnathopod 1. 

Peraeopods 5-7 homopodous, bases broad. Uropod 3, 
inner ramus narrowly lanceolate, length ~2X peduncle , with 
5-6 marginal spines; outer ramus short -60% of outer ramus, 
with a few marginal spines distally. 

Telson relatively short, length -1.5 X width, apex 
broadly acute. 


Distribution. Bering Sea and coast of Kamchatka, 

subtidally on Alariafistulosa. Strictly Asiatic Pacific. 

Taxonomic commentary. The species is plesiomorphic 
in most character states but is distinct in the weakly spinose 
rami of uropod 3, and very broadened palp of maxilla 1. 

Chromopleustes lineatuSf new species 
(Figs. 9, 10) 

Parapleustes oculatus Bousfield, 1985, part. 

Material Examined. About 25 specimens in 10 lots: 
ALASKA. 

Southeastern Alaska: ELB Stn. A171 (Puffin Bay, Baranof 
I.), rock and algae at LW level, July 25, 1961 - 22 im.; ELB 
Stns., July, 1980: S7B1 (Dry Pass, Chichagof L), under 
boulders, algae, LW - 1 female; SllBl (Column Pt., 
Lisianski Strait), bedrock and kelp atLW, July 30, 1980 - -50 
specimens including males and females. 

BRITISH COLUMBIA. 

North-central coast: ELB Stn. N1 (Rivers Inlet), bedrock. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


79 



FIG. 9. Chromopleustes lineatus, new species. Male (7.5 mm); Female ov (9.0 mm) Ahous Bay, B. C. 

I.), bedrock, Phyllo-spadix, sand, at LW, Aug. 18, 1959 - 
male (7.5 mm), Holotype (slide mount), CMN Cat. no. 
NMCC1995-(X)71; female ov (9.0 mm). Allotype (slide 


Phyllospadix, and coarse sand at LW, Aug. 3, 1959 - 25 
specimens, including males, females, im. 

Vancouver I., north end: ELB Stn. 05 (Ferrer Pt. beach), 
under bedrock and kelp at LW, July 20, 1959 - 6 males 2 
females, 3 im. 

Vancouver I., south end: ELB Stn. 012 (Ahous Bay, Vargas 


mount), CMN Cat. no. NMCC1995-(X)72; 7 males, 3 females, 
Paratypes, CMN Cat. No. NMCC1995-0073. ELB Stns., 
1975: P5c (Taylor I, Trevor channel), from ascidians and 


AMPHEPACIFICA VOL II NO. 1. AUG. 31, 1995 


80 



sponges under large boulders at LW level, - 1 male. ELB 
Stns., 1976: B7 (Broken Is., Trevor Channel), from sponges 
under rock, LW level - 9 males 6 females, 6 im. ELB Stns., 
1977: Bllb (Wickaninnish Bay, south end), from sponges 
and algae under steep bedrock walls at LW - 1 male, 2 
females; B13 (Trevor channel, off Brady’s beach), 6-14 m 
dredge, sand, stone, algae - 1 female ov (14 mm); B14 
(Trevor channel, off Execution rock), 44-54 m dredge, sandy 
mud, algae - 1 female ov. 


CALIFORNIA. 

Albion Cove, Mendocino Co., from Tealia species, 20 m 
depth, T. Chess coll., Sept. 26, 1978 - 1 10 females, 20 males. 

Diagnosis. Male (7.5 mm): Head, eye broadly ovate, 
black in alcohol. Antenna 1, flagellum ~60-segmented; 
accessory flagellum minutely subconical, with 3 apical 
setae. Antenna 2, peduncular segment 5 little longer than 4; 
flagellum ~35-segmented. 


81 


AMPHIPACIFICA VOL II NO. 1 . AUG. 31, 1995 



^O.n.CommensipUus,escommensalU (Shoemaker). Female ov (5.5 mm). Point Barrow, Alaska. 
(after Shoemaker, 1952). 


t U v-cleft separating asymmetrical 

lobes. Lower lip, inner lobes broad, flat. Mandible, spine 
row with 11-13 slender blades plus supernumerary setae; 
right incisor with 9, left incisor with 1 7 stout teeth; left lacinia 
with ~20 teeth, distally smallest; palp segment 3 with 10 
pectinate “D” spines (of Cole, 1980) and 3 longer apical 
setae. Maxilla 1 , inner plate with single short apical setae; 
outer plate with ~18 slender apical spines; palp segment 2 
apically rounding, with 8-9 short spines. Maxilla 2, outer 
plate broader than inner. Maxilliped, inner plate with large 
inner marginal blade-like spine and 4 small apical denticles; 
outer plate rounded apically; palp segment 1 shorter than 2 
Coxae l-3relativelybroad,deep. Gnathopods distinctly 
sexually dimorphic. Gnathopod 1 , posterior margin of basis 
acking distinct proximal “hump”; carpus short, as deep as 
long; propod relatively deep, length ~ 1.5 X depth, palm 
oblique, nearly straight, postero distal angle with 4 groups of 
spines extending onto posterior margin. Gnathopod 2 , 
propod very short, length distinctly less than depth; propod 
larger than in gnathopod 1 , slightly broadening distally, 
palm oblique nearly straight, posterior angle with 4 spine 
clusters and adjacent single small spine on posterior margin; 
dactyls with minute posterior marginal setules. 

Peraeopods 3 & 4, segment 6 relatively short, hind 
margin with 6-7 spine clusters. Peraeopods 5-7 homopodous 
peraeopods 5 slightly the shortest; basis of peraeopod 5 less 
broadly expanded than in 6 & 7; dactyls medium, gentlv 
curved distally. 


Pleon side plate 3 , hind comer acuminate ; uropods 1 &2 
slightly shorter and less strong than in C oculatus\ inner 
ramus of uropod 1 with 6-8 serial paired spines. Uuropod 2 
Uropod 3, inner ramus, length ~-2X peduncle, margins with 
8-9 serially paired spines 

Telson medium, length 1.5 X width, apex subtruncate. 

Female (9.0 mm): Slightly larger and heavier- bodied than 
male. Gnathopod 1 . carpus slightly longer, length slightly 
greater than depth; propod shorter, length ~ 1.3X depth. 
Gnathopod 2 , carpus not shortened, length -1.5 X depth- 
propod subrectangular, not broadening distally. 

Distribution. From southeastern Alaska, through the 

Queen Charlotte islands and north central mainland coast of 
Bntish Columbia to Mendocino Co., northern California 

oftenin association withsponges,coelenterates and tunicates’ 

on hard bottoms, from LW level in the north, subtidally to 
depths of over 50 m in the south. 

Etymology, from the Latin meaning lined, al- 

luding to the fine, orange, dorso-lateral body stripes, and 
vencal yellow stripes on brownish coxal plates 1 - 4 . 

Taxonomiccommentary, Thespecies differs markedly 
from C oculatus in colour, and from C. johanseni in char- 
acters of the key (p. 74), and additonally in the highly 
modified mouthparts, especially the mandible and maxilla 1 . 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


82 


Commensipleustes, new genus 

Parapleustes Shoemaker, 1952: 231. — J. L. Barnard, 1969a: 
(partim). — Barnard & Karaman, 1991: 650. 

Type specis. Parapleustes commensalis Shoemaker, 1952: 
231, fig. 83. (see Fig. 11). 

Diagnosis. Head, rostrum about equal to rounded 
anterior lobe. Eyes medium large, black. Antennae slender, 
peduncles short, flagella short (<15 segmented). 

Upper lip, medium notch shallow, lobes slightly 
asymmetrical. Lower lip inner lobes deep medium wide, 
rounded; outer lobes small, ovate, oblique. Mandible, molar 
process relatively strong, apex slightly triturative(?); spine 
row with numerous (10+) blades; left lacinia 10-dentate; 
palp segment 3 slender, with 2 inner marginal pectinate “D” 
spines. Maxilla 1, inner plate small, with single apical seta; 
palp segment 1 lacking shoulder seta(e) segment 2 stout, 
apex obliquely rounded, with 8 short spines, and a facial row 
of 3 setae. Maxilla 2 , inner plate regular, with single inner 
marginal plumose setae. Maxilliped, inner plate with 3 
apical “button” spines and 2 slender spines; outer plate, apex 
with 2 slender spines, segment 3 lacking distal pectinations; 
palp relatively short, curved. 

Coxae 1-3 relatively narrow, 1 not expanded distally. 
Lower margins gently convex, hind cusp minute. Coxa 4 not 
broader than deep. Gnathopods medium strong, closely 
subequal, not sexually dimorphic (?). Gnathopod 1, basis, 
anterior margin strongly short-setose; hind margin weakly 
so merus lacking distal process; carpus, hind lobe relatively 
broad, rounded below; propod relatively short, not expanding 
distally; palm oblique, convex, median tooth apparently 
lacking. 

Peraeopod 3 & 4, basis, antero-distal margin with short 
setae; segment 5 short, length < segment 4; segment 6 stout, 
hind margin distally with groups of stout spines against 
which the dactyl closes, forming a grasping organ. Peraeopods 
5-7 homopodous, short, stout; bases medium; segment 5 
short; segment 6, anterior marginal spines and dactyl forming 
a grasping organ, as in peraeopods 3 & 4. 

Pleon plates 2 & 3, hind comers mucronate, slightly 
produced. Uropods 1 & 2, relatively short, little or not 
exceeding uropod 3. Uropod 3, inner ramus relatively long. 

Telson linguiform, medium, distally narrowing to 
rounded apex. 

Distributional ecology. Commensipleustes commens- 
alis, the only known species, occurs on pleopods of the spiny 
lobster, Panulirus interruptus, off Santa Barbara, CA. Also 
recorded by Wicksten (1982) off southern California. 

Taxonomic commentary. The prehensile peraeopods, 
in combination with the short peraeopodal segment 5, 
unexpanded coxa 1, and specialized mouthparts are here 
deemed sufficient for separate generic recognition. 


Gnathopleustes, new genus 

Parapleustes Guijanova, 1972: 131 (part).— Barnard, 1969b: 
203 (part).— Barnard & Karaman, 1991: 649 (part). 
Neopleustes Stebbing, 1906: 311 & 728 (part). 
Parapleustinae, group 1 (part) Bousfield & Hendrycks, 
1994: 42. 

Type species. Iphimedia pugettensis Dana, 1853, original 
description. 

Species. Gnathopleustes serratus, new species (= 
Parapleustes pugettensis Shocmdker, 1964); G. den (Barnard, 
1969b); G. pachychaetus, new species; G. trichodus. new 
species; G. simplex, new species. 

Diagnosis. Body smooth above. Head, rostmm shorter 
than bluntly rounded anterior lobe; inferior antennal sinus 
broadly incised. Eyes medium large, subrotund. Antennae 
well-developed; posterior margins often setose. Antenna 1 
the longer, peduncular segment 2 short; accessory flagellum 
minute, apex 2-3 setose. Antenna 2, peduncle strong, 
flagellum often with special thickened setae. 

Mouthparts strongly modified. UL shallowly notched, 
lobes asymmetrical. Lower lip broad, outer lobes rounded, 
oblique. Mandible: incisor regularly toothed; left lacinia 7- 
10 dentate; blades 4-12 in number, stout, distally chisel- 
shaped; molar body reduced, slender, apex fuzzy; palp 
normal, segment 1 short, segment 2 medially setose. Maxilla 
1, outer plate with 9 tall slender apical spines; palp with 
subapical facial setae. Maxilla 2, inner plate little expanded; 
maxilliped, palp strongly dactylate, segment 2 largest; outer 
plate segment longer than palp segment 1, not enormously 
developed; inner plate short, inner marginal setae numerous 
(4-9). 

Coxal plates wide, deeper than corresponding body plates; 
coxa 1 broadened distally, hind margin spinose near basis, 
postero-distal notch single, small. Gnathopods 1 & 2 large, 
subequal (Gnathopod 2 larger), variously sexually dimor- 
phic; basis stout, with antero-distal setal group; merus with 
slight distal process; carpus, posterior lobe short, deep (esp- 
ecially in male); propods subovate, palms strongly oblique, 
elongate, convex, palmar tooth distinct, near hinge; palmar 
margin tending to be lined with special thickened or blade- 
like setae; postero-distal angle with 2-4 groups of spines, 
hind margin short, bare, or longer, setose. 

Peraeopods 3-7 stout, spinose, normal; segment 5 strong, 
moderately overhung proximally by segment 4; dactyls 
medium strong, curved. Peraeopods 3 & 4, margins of 
segments 4, 5 & 6 may bear special thickened setae. 
Peraeopods 5-7 regularly homopodous, bases broad, convex 
behind. 

Pleon side plates broad, deep, hind comers acuminate but 
not strongly produced. Pleopods strong, normal, not sexu- 
ally dimorphic. Urosome short, segment 2 nearly occluded 
dorsally. Uropods 1 & 2 regularly spinose; uropod 1, rami 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


83 


KEY TO KNOWN SPECIES OF GNATHOPLEUSTES 


moderately to strongly setose posteriorly; gnatho- 

pods tending to strong sexual dimorphism, palmar margins heavily lined with blade-setae or split-tipped 

°n^ f -50% length of antenna 1, flagellum ne^iy bare (short seMe'only);' gnathopods 
pods slightly sexually dimorphic, palmar margins lined with relatively few normal setae 5. 

margins heavily lined with split-tipped setae; mandible, blade 
row of 10-12 unmodified blades; antenna 1 (male), flagellum brushy G. simplex, (p 87) 

-Gnathopods (male), m^gms lined with “balloon" setae (pachychaete); mandible, blades (especially dist 
a y) modified, antennal setation weak, with no distinct “brush” (setose on hind margin only) 3. 

^'stronglyletotr'*' 5-7 all lacking marginal setae; gnathopod palms 

-Antenna peduncles spinose and setose (flagella of A2 variously setose); peraeopods 3-4 oi ^7 sJonglv 
setose behind; gnathopod palms strongly setose (with “balloon” setae) 4 


4 . Gnathopod 2, palmar margin distinctly concave, postero-distal angle with 2 spine groups; peraeopods 
■ti Q of segments 4-6 with clusters of long brushlike setae (male); uropod 3, outer ramus 

with 6-9 nwgmal spines; antenna 1, peduncular segment 1 not elongate G. trichodus (p 91) 

-Gnathopod 2. palmar margin nearly straight, postero-distal angle with 3-4 spine clusters; peraeopods 5- 
7, hind m^gins of segments 4 - 6 with spine clusters only (lacking setae); uropod 3, margins of outer 
ramus with 5-7 spines only; antenna 1, peduncular segment 1 long G. pachychaetus (p. 87) 


5 Gnathopods, dactyls smooth behind; telson less than twice as long as wide; peraeopods 5-7, segment 5 

^stinctly shorter than 4, strongly overhung posteriorly by segment 4 G, pugettensis (p. 83) 

Gnathopods, dactyls postenorly finely serrate; telson elongate, at least twice as long as wide; peraeo- 
pods 5-7, segments 4 & 5 subequal in length, 5 normally overhung by 4 G serratus (p 91) 


subequal; uropod 2, outer ramus the shorter. Uropod 3, outer 
ramus distinctly the shorter. Telson elongate, narrow- 
ingdistally; dorsal penicillate setae about mid-point from 
base. Coxal gills large, broad. 

Taxonomic commentary. Members of Gnathopleustes 
overlap to considerable degree with members of Inciso- 
calliope . However, the two genera are maintained as distinct 
units for the present because they can be keyed, and the 
distributions are discreet. Within Gnathopleustes, two main 
subgroups Can be distinguished, as outlined in the key below. 
In the more advanced members (G. pugettensis, G. den, G. 
simplex) the gnathopods appear very slightly sexually dimor- 
phic, and the mouthparts, peraeopods and uropods are apo- 
morphic. 


Parapleustes pugettensis Barnard, 1969b: 203.— Austin, 
1985:592. — Staude, 1987:379. — Barnard &Karaman, 1991- 
650. 

TmJncisocalliope newportensis Barnard, 1959: 22. 

1^ Parapleustes pugettensis Barnard & Given, 1960:43. 
— Ishimaru, 1984: 19. 

Material examined. 258 specimens in 38 lots- 
ALASKA. 

Southeastern Alaska. ELB Stns, June- July, 1961: A40 (4 + 
slide mount); A80 (1); A164 (1); A171 (1). 

BRITISH COLUMBIA. 

Queen Charlotte Islands. ELB Stns., July-August 1957- 
Wll (6) W15b(l). 


Distributional commentary. Members of the genus are 
restricted almost entirely to the Pacific coast of North America, 
from southeastern Alaska to southern California! 
Gnathopleustes pugettensis has been reported, but not 
confirmed, from Japanese waters by Irie & Nagata (1962). 

Gnathopleustes pugettensis (Dana) 

(Fig. 12, 13) 

Iphimedia pugettensis Dana, 1853: 932, pi. 63, fig. 6. 

Neopleustes pugettensis Stebbing, 1906:728. 


North-central coast, ELB Stns., July, 1964- H43 (!)• H53 
(1);W64(2). 

Northern and central Vancouver I.: ELB Stns., 1959: HIO 
(40 specimens including males and females); N16 (1); V4b 
(Hope I., Roller Bay), under boulders, kelp, Phyllo-spadix, 
at LW level - male (slide mount) (fig'd specimen); female 
(slide mount) (fig'd specimen) + 8 other specimens; VIO(IO)- 
V17(1);V19(1). 

Southern Vancouver I.: ELB Stns., 1955: P9(l) ELB Stns 
1970: P702 (20); P707 (5); P710b (1); P714 (1); P719 (5,' 
including females ov.). ELB Stns, 1975: P2 (25); P3a (1); 
P5a (1); P5b (1). ELB Stn. B4 , off Brady’s Beach, 60-70 m 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 84 



FIG. 12. Gnathopleustes pugettensis (Dana). Male (4.0 mm). Southern California, 
(modified from Barnard & Given (1960). 


naturalist’ s dredge, sand and algae, June 25, 1976 - 2 females. 
ELB Stns., 1977: B8 (5); B 14(1). 

WASHINGTON-OREGON: 

Strait of Juan de Fuca to Newport. ELB Stns., July-Aug., 
1966: W22 (30, including slide mount); W30 (1); W34 (1 1); 
W35 (9); W36(8); W40 (19); W50 (30, + slide mount); W53 
(1); W57(l); W63 (6);W66 (2). 

Diagnosis. Male (6.0mm); Body relatively short, coxal 
and pleon plates deep. Head, eye large, subrectangular. 
Antenna 1 , peduncular segment 3 relatively long (1/2 segment 
2); flagellum of 35-40 medium long segments; accessory 
flagellum conical, apex with single long seta. Antenna 2, 
peduncular segment 5 shorter than 4; flagellum with ~35 
nearly marginally smooth segments. 

Upper lip strong, asymmetrical. Lower lip, inner lobes 
deep; outer lobes normally oval, oblique. Mandible, molar 
short, blunt; spine row with 8-10 stout, abruptly acute 
blades; incisor, cutting edge with 6 uneven teeth; palp seg- 
ment 3 with 8 inner marginal pectinate spines; left lacinia 
with 8 unequal teeth. Maxilla 1, palp segment 2 with 4 
unequal apical spines. Maxilla 2, outer plate not narrowing 
distally, apex strongly setose. Maxilliped, inner plate rel- 
atively large, distally broad, with 7 distal facial setae, and 4 


small apical marginal denticles; outer plate regular, apex 
subtruncate; palp, dactyl slender, curved. 

Coxae 1-3 relatively large, deep; coxa 5 deep. Gnathopod 
1 , carpus medium, about as deep as long, carpal lobe medium; 
propod smoothly ovate, palmar margin convex, very oblique, 
postero-distal angle with groups of 4 and 3 spines and a 
single spine distally on posterior margin; dactyl, hind margin 
not serrated, with a few setules only. Gnathopod 2, carpus 
and dactyl slightly larger, but proportions and armature 
similar to that of gnathopod 1. 

Peraeopods 3 & 4 relatively short, distal segments (4/6) 
weakly marginally spinose; dactyls medium, > 1/3 length of 
segment 6. Peraeopods 5-7 closely homopodous, 5 slightly 
smallest; bases broadly expanded, hind margins convex; 
distal segments (4-6) weakly marginal spinose, not setose; 
dactyl medium. 

Pleon plates 1-3 deep, broad, hind comer of 3 squared. 
Urosome 2 occluded dorsally by 1 & 3. Uropods ordinary. 
Uropod Lpeduncularpostero-distal spine strong. Uropod2, 
outer ramus short, length ~2/3 inner ramus. Uropod 3 strong, 
inner ramus >2 X peduncle, margins with 5 spines. 

Telson subrectangular, length about 1.5X width, apex 
truncate. 

Female (5.5 mm): Gnathopods not described, presumably 
slightly smaller and less setose than in male. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 



FIG. U.Gnathopleustespugettemis (Dana). Male (6. 0 mm). RoMerBay. B. C 


Distribution. From southeastern Alaska and northern 

British Columbia south through Washington & Oregon to 
Point Conception and Santa Barbara regions, subtidally to 
70 m; replaced by /. newportensis south of Pt. Conception. 

Taxonomic commentary. Gnathopleustes pugettensis 
is the generic type and, in balance of character states, is most 
advanced. Overall, it is closely similar to G. den and G. 
simpleA. 


Gnathopleustes den (Barnard) 

(Fig. 14) 

Parapleustes den J. L. Barnard, 1969b: 199, fig. 54 — 
Staude, 1987: 319. — Barnard & Karaman, 1991: 650. 

Material examined. Male (8.0 mm), Holotype, J. L. 
Barnard Stn. 6, Allan Hancock Foundation Cat No. #559. 
Material of this species was not found in the study range, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


86 



FIG. 14. Gnathopleustes den (J. L. Barnard). Male (8. 0 mm). Corona del Mar, California. 

(after Barnard, 1969b). 


despite its close similarity to G. pachychaetus. 

Diagnosis (partly after Barnard 1969b). Male (8.0 m): 
Body and coxal plates medium, ordinary. Head, eyes medium, 
broadly short-reniform. Antenna 1, peduncular segment 3 
medium, length 1/2 segment 2; accessory flagellum very 
short, with 2 slender apical spines; flagellum elongate (59 
segments). Antenna 2, peduncular segment 5 not shorter 
than 4; flagellum with 50+ segments, proximally stoutest, 
nearly bare. 

Upper lip, apical cleft relatively deep, lobes nearly 
symmetrical. Lower lip, inner lobes deep, outer lobes 
steeply oblique. Mandible, molarprominent, apex subacute?; 
spine row with 13-15 medium stout blades; left lacinia 9- 
dentate; cutting edge of incisor with 6 irregular teeth; palp 
segment 3 with 11-12 inner marginal pectinate “D” spines. 
Maxilla I, palp, apex with 6-7 spines. Maxilliped, inner 
plate with 1 marginal spines and 2 facial setae; outer plate 
tall, columnar. 

Coxal plates 1-3 large, deep, relatively narrow; coxae 1 
distally expanding, 1-3 with 3-4 hind marginal spines; coxa 
5, lobes medium deep. Gnathopod 1 , c£upus medium, length 
and depth subequal; propod ovate, palmar margin shallowly 
oblique, very slightly convex, densely finely setose, 
continuous with hind margin, median tooth very weakly 
developed; postero-distal angle with 3 groups of spines (?); 


dactyl stout, hind margin smooth, not serrated. Gnathopod 
2, propod distinctly larger and deeper than in gnathopod 2 ; 
palm nearly horizontal, nearly straight, densely finely setose, 
with weak median tooth, postero-distal angle with 3 groups 
of spines, a single distal spine on the posterior margin; dactyl 
stout, smooth behind. 

Peraeopods 3 & 4 strong; segment 6, hind margin with 
6 spine groups; dactyl short. Peraeopods 5-7 relatively stout; 
bases slightly broadest distally, hind margins nearly straight, 
weakly crenulate; segment 4 broad, width -2/3 length; 
segment 6, margins spinose (not setose); dactyls medium, - 
1/3 length of segment 6. 

Pleon plate 3, hind comer acuminate. Urosome2 with 
free dorsal margin. Uropods 1 & 2 stout, rami relatively 
short, not extending beyond uropod 3; uropod 2, rami 
subequal. Uropod 3, inner ramus with 6-7 pairs of marginal 
setae. 

Telson subrectangular, length ~ 2X width, apex 
subtruncate. 

Female (10.0 mm); Undescribed. 

Distribution. Known only from the type locality at 
Corona del Mar, south of Pt. Conception, California, in 
washes of tubes of the polychaete Phragmatopoma sp., at 
LW level. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


87 


Taxonomic commentary. The type male specimen, 
figured by Barnard (1969b), differs from G. pachychetus in 
lacking posterior marginal setae on the peduncle of antenna 
1, and in lacking brush setae on the flagellum of antenna 2. 

Gnathopleustes simplex, new species 
(Fig. 16) 

Material examined. 

BRITISH COLUMBIA: 

Southern Vancouver Island: Off Wouwer I., Barkley Sound, 
P. Lambert coll., June 29, 1973 - male Holotype (6.8 mm) 
RBCM loan No. 973-156. 

ELB Stn P17d, Kirby Pt. Bay, Diana I., under-rock habitat 
among sponges, tunicates, at LW, Aug. 6, 1975- 1 female 
ov. (5.0 mm). 

Diagnosis. Male (6.8 mm). Body slender coxal and 
pleonal plates relatively small, shallow. Head, eye medium 
small, broadly reniform. Antenna relatively short, 1 slightly 
longer than 2. Antenna 1 , peduncular segment 3 short, length 
1/2 segment 2; accessory flagellum minute, conical; flagellum 
with 35 segments, nearly devoid of marginal setae. Antenna 
2, peduncular segments 4 &5 short, 5 slightly longer, both 
with facial clusters of setae; flagellum of 30 weakly brush- 
like segments, basally stoutest, each with distal cluster of 
short setae. 

Mandible, molar small apically conical; spine row with 
10-11 slender blades and a few supernumerary setae; cutting 
edge of incisor with 6 variably sized teeth; palp segment 3 
short, inner margin with 1 1 pectinate “D” spines; leftlacinia 
with 12(?) teeth. Maxilla 1, palp slender with 4 apical slender 
spines? Maxilla 2? Maxilliped, inner plate short, broadest 
medially, with distal facial setae, and 4? apical marginal 
spinules; outer plate relatively short, distally narrowing, 
apex rounded; palp, dactyl curved. 

Coxae 1-4 medium, 1 & 2 each with 2-3 posterior 
marginal spines. Gnathopod 1, basis with antero-distal 
marginal setae; carpus short, deeper than long, hind lobe 
distally broad; propod short ovate, relatively deep, palmar 
margin shallowly oblique, nearly straight, moderately 
marginally simple-setose, with distinct median tooth, postero- 
distal angle with cluster of 3 spines, posterior margin with 
single distal cluster of 2 spines; dactyl smooth behind. 
Gnathopod 2 similar, but large; basis with fewer antero- 
distal setae; carpus, hind lobe slightly broader; propod more 
elongate, palmar margin slightly concave; postero-distal 
angle with cluster of 3 spines; hind margin strongly setose, 
with distal cluster of 3 spines; dactyl smooth behind. 

Peraeopods 3 & 4 ordinary, not setose; dactyls medium. 
Peraeopods 5-7 bases not strongly broadened, hind margins 
nearly straight; segment 4 short; segments 4-6 anterior and 
posterior strongly spinose and setose; segment 6, anterior 
margin with 6-7 clusters of spines and setae; dactyls medium. 

Pleon plate 3 weakly spinose below, hind corner 
acuminate. Urosome 2 occluded dorsally by segments 1 & 

3. Uropod 1 , rami not elongate, weakly spinose marginally. 


Uropod 2, outer ramus distinctly the shorter. Uropod 3 
regular(?). Telson medium, narrowing distally 7 to sharply 
rounded apex. 

Distribution. Known only from Barkley Sound, 
Vancouver I., British Columbia, LW and shallow subtidally, 
associated with sponges and tunicate, under rocks. 

Etymology. From the Latin “simplex”, meaning simple, 
not ornate, with reference to the unshortened, unbroadened 
blades of the mandibular spine row. 

Taxonomic commentary. Gnathopleustes simplex 
encompasses some plesiomorphic character states (e.g., slen- 
der mandibular blades) but, in balance of character states, is 
apomorphic. It appears not unlike G. pugettensis and the 
more southerly G. den, in the form of the antenna and other 
features of the mouthparts, especially the maxilliped. 

Gnathopleustes pachychaetus, new species 
(Figs. 17,18) 

Material examined. 

ALASKA. 

Southeastern Alaska. ELB Stns., June-July, 1961: A6 (1); 
A8(4 + slide mount); ABO (4); A171 28 + slide mount). 
ELB Stns, July, 1980: S4B4 (2); SllBl (2); S18B1 (!)• 
S22F1 (1). 

BRITISH COLUMBIA. 

Queen Charlotte Islands. ELB Stns., July- August, 1957: E21 
(3); W9 (4). Flamingo Harbour, Stn. 3539, July 17, 1935 - 

4 females ov; J FRB Stn. Ml-65-55, DBQ, JWS coll., Aug. 
6, 1965 - 1 female ov. 

North-central coast, ELB Stns., July, 1964: H35 (-lOO)- H39 
(15); H40 ~70); H41 (-25). 

Northern and central Vancouver I.: ELB Stns, July, 1959: 

05 (-15); 017 (7); N18 (17, incl. males and females). R. M. 
O’Clair Stns, 1976: #760007, Kelsey Bay (1 male; # 
760023, Squirrel Cove, Cortez I. - 30 males and female (+ 
slide mount); #760046, Port Hardy - 1 female ov. 

Southern Vancouver I.: ELB Stns, July-August, 1955: P4 
(~15); P6a(-40)P6c(-15);F5 (-15); Ml 1 (-30). ELB Stns, 
1970; P704 (1); P702 (1); P707 (-25); P708 (1). ELB Stns, 

1 975 : P 1 7d ( 1 female + slide mount); P5c (5); P20a ( 1 ); P20c 
(2). ELB Stns., 1976: B 1 (10); B2 (6); B4 (9); B5 (44); B7 (2); 
B8(l);B12b(-160+ slide mounts); B 1 3 (-30)B28 ( 1 ). ELB 
Stns, 1977: B6a (3); B8 (1): B1 la (1); Bllb (2); B13 (1); B 
19b(2). R. M. O’Clair Stns., 1976: #760028, Sturdies Bay, 
Galiano I. - 9 males Sc females. # 760031 Miner’s Bayi 
Mayne I. (-30 males, females). #760034, Horton Bay, Mayne 
I., June 22, 1976 - Male (6.8 mm), Holotype (slide mount), 
CMN Cat. no. NMCC 1995-0076; female (5.8 mm). Allotype 
(sUde mount), CMN Cat. no. NMCC 1995-0077, -i- 8 males, 

12 females, Paratypes, CMN Cat. no. NMCC 1995-0078. ’ 
Ogden Pt. breakwater, Victoria, R. J. Long coll., 1976 - 2 
females, 1 male. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


88 



FIG. 16. Gnathopleustes simplex, n.sp. Male (6.8 mm); female ov (5.0 mm). Barkley Sound, B. C. 


WASHINGTON-OREGON. 

Coastal Stations, ELB, July-August, 1966: W2 (4 + slide 
mount); W5 (2); W22 (9 + slide mounts); W24 (-300); + 
slide mounts); W34 (15) W45 (9); W50(~50); W53 (10); 
W57 (-25); W58 (-28); W61 (23); W63 (-70). 

Eagle Cove, San Juan I., R. M. O’Clair Stn. 74001, June 21, 
1974 - 2 females (slide mount). 

Charleston, Ore., mouth of Coos Bay, floating dock below 
LW, among Enteromorpha and Polysiphonia sp., K. E. 
Conlan coll., July 8, 1986: Stn 07- 1 - -70 males, females, im; 
Stn. 08-23 - 3 females, 4 im. 

Diagnosis. Male (6.8 mm): Body slender, coxal and pleonal 
plates medium deep. Head, eye relatively small, short- 
reniform. Antenna 1 , peduncular segments each with posterior 
marginal clusters of long setae; segment 3 long, length -2/ 
3 segment 2; accessory flagellum cone-like, with strong 
apical seta; flagellum with 48 segments. Antenna 2 shorter 
than 1; peduncular segment 5 not shorter than 4, both with 


posterior and facial clusters of setae; flagellum relatively 

short, with -40 short segments, brush-like posteriorly. 

Upper lip tall, apical cleft shallow, lobes asymmetrical. 
Lower lip, inner lobes deep; outer lobes large, ovate, strongly 
oblique. Mandible, molar small apex subacute; spine row 
with 8-9 short thick blades, cutting edge of incisor with 7 
regular teeth; palp segment 3 narrowing distally , inner margin 
with 1 8 pectinate “D” setae; left lacinia with 8-9-dentate. 
Maxilla 1, palp slightly narrowing distally, with 5 apical 
spines. Maxilla 2, outer plate narrowing distally apex 
relatively sparsely setose; inner plate with stout median 
marginal setae. Maxilliped, inner plate broad, with 7 distal 
facial setae and 5 apical marginal spinules; outer plate tall, 
columnar, apex rounded; palp segment 3 large stout, palp 
slender curved. 

Coxal plates 1-3 each with single posterior marginal 
spine. Gnathopod 1, carpus shorter, deeper than long; 
propod ovate, narrowing distally, palm nearly horizontal 
with distinct median tooth, and dense clusters of long thick 



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89 



90 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 



Fig. 18. Gnathopleustes pachychaetus, new species. Male (6.8 mm). Mayne I., B. C. 


marginal "balloon" setae, margin merging smoothly with 
posterior margin, spine group at postero-distal angle with 4 
spines, outermost largest, posterior margin with single distal 
cluster of 3 spines; dactyl, hind margin with a few small 
setules. Gnathopod 2 very similar but slightly larger, carpal 
lobe slightly deeper; palmar margin relatively short , distally 
slightly concave, postero-distal angle, spine cluster with 4 
spines, posterior margin distally with a single spine and 
single cluster of spines. 

Peraeopods 3 & 4, segment 4-6 with dense clusters of 
spines and setae especially posteriorly; dactyls medium. 
Peraeopods 5-7 similar, bases slightly broadening distally, 
hind margins gently convex; segment 5 short, segment 6 


long, margins spinose, not setose; dactyls medium. 

Pleon plates 2 and 3, lower margins weakly spinose, 
hind comers acuminate, slightly produced. Urosome 2 
occluded dorsally by segments 1 &3. uropods 1 & 2 slender, 
slightly exceeding uropod 3 . Uropod 2 , outer ramus distinctly 
shorter than inner ramus. Uropod 3 , inner ramus with 6 pairs 
of marginal spines, outer ramus relatively large, = 3/4 inner 
ramus, margins 5 -spinose 

Telson broadly linguiform, apex broadly rounded. 

Distribution. From southeastern Alaska, commonly 
throughout B. C. coastal waters, to southern Oregon, under 
rocks and among algae at LW level to shallow subtidal. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


Etymology. From the Greek root words "pachy", 
meaning thick, and '"chaite" meaning hair, in reference to the 
thick, broad, laminate setae comprising the setose armature 
of the gnathopods. 

Taxonomic commentary. Gnathopleustes pachy- 
chaetus is somewhat similar to the more southerly species, 
G. den, in the strongly setose, weakly sexually dimorphic 
gnathopods, and in some mouthparts (e.g., mandibular 
blades). However, the gnathopod setae are more strongly 
thickened, and thick setae occur also on the distal se gm ents 
of the peraeopods, especially in the male. The posterior 
margins of peduncular segments of antenna 1 have 6-8 clust- 
ers of strong setae, and the flagellum of antenna 2 is brush- 
like, whereas corresponding parts of G. den are bare. 


Gnathopleustes trichodus, new species 
(Fig. 19) 

Material Examined. 

BRITISH COLUMBIA. 

Southern Vancouver I.; West of Amphitrite Point, N. A. 
Powell Stn 67-83, 22 m, Aug. 22, 1967 - male Holotype 
(slide mount) CMN Cat. no. NMCC 1995-0083. 

Diagnosis. Male (8. 5 mm): Body slender, coxal and 
pleonal plates medium deep. Head, eye broadly reniform, 
black. Antenna 1 shorter than antenna 2; peduncular 
segment 3 short, length< 1/3 segment 3; accessory flagellum 
conical, with 1 large apical setae; flagellum with 55 segments 
basally slightly short-setose. Antenna 2, peduncular segment 
5 longer than 4, both with distal and facial clusters of setae; 
flagellum elongate, with -50 segments, each with prominent 
distal whorl of short setae. 

Upper lip, median notch shallow, lobes nearly 
symmetrical. Lower lip, inner lobes relatively shallow, outer 
lobes regularly ovate, oblique. Mandible, molar process 
prominent, apex subacute; spine row with 9 medium stout 
blades, tips obliquely acute; cutting edge of incisor with 6 
irregular teeth; palp segment 3 slender, elongate, with 13 
inner marginal pectinate “D” spines; left lacinia9- 1 0 dentate. 
Maxilla 1 , palp slender, with 4 apical spines. Maxilla 2, outer 
plate distally narrowing, apex strongly setose. Maxilhped, 
inner plate short,, with 7 distal facial setae and 5 apical 
marginal short spines; outer plate short narrowing to 
subtruncate apex; palp segment 3, inner margin with pectinate 
setae, dactyl slender, nearly straight. 

Coxal plates 1-3 relatively broad, each with 1-3 hind 
marginal short spines, coxa 4 very broad, width and depth 
subequal. Coxa 5 shallow. Gnathopod 1, carpus short, 
deep>er than long, lobe narrow; propod, palmar margin straight 
or slightly concave, median tooth strong, postero-distal 
angle with 2 groups of spines; median face with numerous 
clusters of slender thickened setae, giving densely setose 
appearance to propod; dactyl strong, not serrated behind. 
Gnathopod 2, similar, larger, very heavily setose; palm of 


propod distinctly concave; dactyl stout, nearly smooth behind. 

Peraeopods 3 & 4, stout, margins of segment 4-6 setose 
and spinose; dactyls strong, >1/3 length of segment 6. 
Peraeopods 5-7 subsimilar, bases regularly broadly ovate, 
smooth behind; segment 4-6 hind margins strongly setose 
and spinose; segment 4 relatively short; dactyls medium. 

Pleon plate 3, lower margin weakly spinose, hind comer 
acuminate, slightly produced. Urosome 2 nearly occluded 
dorsally by segments 1 & 3. Uropods slender, elongate. 
Uropod 1, distal peduncular spine short. Uropod 2, outer 
ramus slightly shorter than inner ramus. Uropod 3 inner 
ramus slender, margins with 8 pairs of spines; inner ramus 
relatively long, with 5-6 pairs of marginal spines. 

Telson linguiform, medium long, apex broadly rounded. 

Distribution. Known only from the type locality near 
Amphitrite Pt., outer coast of southern Vancouver Island. 

Etymology. From the Greek “trichos” mean hair, 
alluding to the dense setation of the gnathopods and 
peraeopods. 

Taxonomic commentary. Gnathopleustes trichodus 
is a primtive species, phyletically isolate from others of the 
group, especially in the form of the mouthparts, relative 
lengths of the antennae, broad coxal plates, concave gnatho- 
pod palms and densely setose peraeopods. 

Gnathopleustes serratus, new species 
(Figs. 20,21) 

Parapleustes pugettensis Shoemaker, 1964: 410, fig. 10. 

Material Examined. About 40 specimens in 15 lots: 
ALASKA. Southeastern Alaska. ELB Stns, 1961: A75 
(Kayak, Wingham I.), LW, under boulders, June 27 - 5 males 
3 females. 

BRITISH COLUMBIA. 

Queen Charlotte Island. ELB Stns, 1957: W12a(3);Hll(l); 
Stn HI 4a, Yakan Pt., Graham I., under boulders atLW, Aug. 
25 - male (8.7 mm), Holotype (slide mount) CMN Cat. no 
NMCC 1995-0068; female ov. (10.0 mm) Allotype (slide 
mount), CMN Cat. no. NMCC 1995-0069; plus 10 males, 9 
females, 1 im.,Paratypes,CMNCat.no.NMCC1995-0070. 

Northern Vancouver L: ELB Stns N1 (Open Bight, Rivers 
Inlet)(5);V5(NigeiL,)(2). 

Southern Vancouver I.: ELB Stn. 015 (Box I, north end 
Wickaninnish Bay) (20); ELB Stn P719 (Cape Beale), 1970 
- 1 male, 1 im. ELB Stn. B3 (Diana L, Trevor Channel), 1976 
- 1 female. ELB Stn B6a (Trial I. Point, Victoria), 1977 - 4 
specimens 

WASHINGTON-OREGON. 

ELB Stns, 1966: W 40 (4); W57 (2); W58 (4); W61 (1); W63 

(Cape Kiwanda) (>100). 


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FIG. 19. Gnathopleustes trichodus, new species. Male (8.5 mm). West of Amphitrite Pt., V. I., B. C. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


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FIG. 20. Gnathopleustes serratus n. sp. Female (9.0 mm). Dillon Beach, CA. (after Shoemaker, 1964). 


CALIFORNIA. 

Albion Cove, at Cone Rock, Mendocino Co., Tony Chess 
coll., June 29, 1978 - 1 male. 

Diagnosis. Male (8.7 mm): Body relative slender, coxal 
plates shallow. Head, eye large, subrhomboidal. Antenna 1 , 
peduncular segment 3 medium; flagellum with ~45 short 
segments; accessory flagellum, truncate apex with 2 longish 
setae. Antenna 2, peduncular segment 5 not shorter than 4.; 
flagellum with ~25 segments, thickest proximally, each with 
distal ring of short “bottle-brush” setae. 

Upper lip lobes distinctly asymmetrical. Lower lip, 
inner lobes deep, outer lobes short-ovate. Mandible, molar 
prominent, apex blunt; spine row with 8-10 thick, apically 
acute blades; incisor, cutting edge with 6 uneven teeth; left 
lacinia 8-dentate; palp segment 3 with 11-12 pectinate inner 
marginal “D” spines. Maxilla 1, palp stout, with 6 apical 
spines. Maxilla 2, outer plate not narrowing distally, apex 
strongly setose. Maxilliped, inner plate with 10 apical facial 
setae and 3 short apical spines; outer plate tall, distally 
narrowing; palp, dactyl slender, nearly straight. 

Coxae 1 & 2, hind margin with 1-2 median short spines; 
coxa 4 shallow, broad. Gnathopod 1, carpus shorter than 
deep, hind lobe narrow; propod ovate, palm very oblique, 
gently convex, postero-distal angle with groups of 3 & 4 
spines; dactyl strongly denticulate or serrated along proximal 
2/3 of inner margin. Gnathopod 2, carpus short, hind lobe 

smaller than in gnathopod 1 ; propod long-ovate, very oblique 


palm merging smoothly with hind margin, not heavily 
marginally setose; postero-distal angle with 2 groups of 4 
spines; dactyl serrated behind. 

Peraeopods 3 & 4, segments regularly spinose; segments 
5 , hind margin with 5 clusters of short spines; dactyls short. 
Peraeopods 5-7 closely homopodous, 5 slightly shortest; 
bases broadly expanded, hind margin strongly convex, 
minutely serrulate; segment 5 distinctly shorter than 4; 
dactyls short. 

Pleon plate 3, hind comer acuminate. Urosome 2 nearly 
totally occluded dorsally by segment 1 & 3. Uropod 2, outer 
ramus 2/3 length of inner ramus. Uropod 3, inner ramus with 
5 serially paired marginal spines. Telson linguiform, relat- 
ively narrow, length nearly twice width, apex sharply rounded. 

Distribution. From southeastern Alaska to central 
California (Dillon Beach), mostly under boulders, associated 
with sessile invertebrates, Egregia, Corallina and other 
algae, at LW level. 

Etymology. From the Latin ^'serratus", with reference 
to the serrated hind margins of the gnathopod dactyls. 

Taxonomic commentary* Gnathopleustes serratus is 
relatively primitive species in characters of the mouthparts 
(maxilliped) and gnathopods (serrated dactyls), and near the 
base of the genus phyletically. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


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FIG. 21. Gnathopleustes serratusy new species. Male (8. 5 mm); female (10.0 mm). Graham I., B. C. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 
Incisocalliope J. L. Barnard 


95 


Incisocalliope }. L. Barnard, 1959: 22. 

Parapleustes Gurjanova,1951: 645 (part.).— Barnard & 
Given, 1960: 42 (part.).— Guijanova, 1972; 131 (part.).— 
Watling & Maurer, 1973: 1 (part).— Barnard & Karaman, 
1991: 649 (part).— Ishimaru, 1994: 46 (part). 

Parapleustes (derzhavini group) Ishimaru, 1984:407,450. 

Type species. Incisocalliope newportensis Barnard, 1959, 
original designation. 

Species composition. Incisocalliope dilatatus (Ishi- 
maru, 1984); /. bairdi (Boeck, 1871); /. derzhavini 
(Gurjanova, 1938); I. nipponensis, new species; /. makiki (J. 
L. Barnard, 1970); /. aestuarius (Watling & Maurer, 1973); I. 
filiaris (Hirayama, 1988). 

Diagnosis. Body small to medium, slender, smooth 
above. Head, rostrum short, little exceeding rounded ante- 
rior head lobe. Eye small, medium rounded to ovate. Antennal 
flagella slender, nearly bare; antenna 1 longer than antenna 
2. Antenna 1, peduncular segments 2 & 3 short, peduncle 1 
lacking postero-distal cusp; accessory flagellum minute, 
triangular. 

Mouthparts modified. Upper lip, median notch deep, 
lobes asymmetrical. Lower lip broad, squat, outer lobes 
steeply oblique. Mandible, molar reduced to a small setulose 
knob; left lacinia 9-12 dentate; blades numerous (9-14), 
unmodified; incisors 8-dentate; palp segment 2 medially 
sparsely setose, segment 3 longest, apically truncate, segment 
1 medium. Maxilla 1, inner plate with 1 apical seta; outer 
plate with 9 medium strong pectinate spine-teeth; palp not 
broadened, surface setulose, apex rounded, with few spines, 
segment 1 with lateral seta(e). Maxilla 2, inner plate little 
broadened, inner margin with single large plumose seta. 
Maxilliped, inner plate with few (2-4) “button” spines; seg- 
ment 3 longer than palp segment 2; outer plate columnar, 
palp segment 3 largest, segment 3 often with short inner 
distal spine-teeth; dactyl slender. 

Coxal plates 1 -4 medium deep; coxa 4 largest & strongly 
excavate behind; coxa 1 shortest, slightly expanding distally ; 
hind cusps small, single or double. Gnathopods 1 & 2, 
variously (mainly strongly) subchelate, subequal, not sexually 
dimorphic. Gnathopod 1, basis normal, anterior margin 
often strongly setose; meral process weak; carpus short, 
deep; propod, palm convex, with median tooth, not continuous 
with weakly setose posterior margin; postero-distal angle 
with 2-3 spine groups not extending onto palm. 

Peraeopods of medium length and stoutness, segments 
spinose but not setose; segment 4 slightly longer than and 
distally overhanging segment 5; dactyls medium, curved. 
Peraeopods 5-7 homopodous, increasing slightly posteriorly; 
coxae medium deep, rounded behind; bases broad, hind 
margin nearly flat. 

Pleon segments normal, hind comers acuminate (but not 


hooked), lower margins lightly spinose. Pleopods normal, 
not sexually dimorphic, rami medium strong. Uropods 1 & 
2 extending to or beyond uropod 3, rami spinose. Uropod 1 , 
inner ramus slightly the longer. Uropod 2, outer ramus 
distinctly the shorter. Uropod 3, rami relatively short, inner 
ramus distinctly the longer. 

Telson medium long, keeled proximally below, apex 
rounded, with small paired notch and seta. 

Coxal gills undescribed. Brood plates large, broad. 

Taxonomic remarks. Incisocalliope is phyletically the 
most advanced genus, with closest relationships to Gnatho- 
pleustes and, to some extent, to Trachypleustes. These 
groups may be distinguished by a combination of character 
trends, as outline in the key and Table I. (p. 128). 

Distributional ecology. Species of Incisocalliope occur 
mainly in temperate or subtropical regions of pan-Pacific 
and North Atlantic regions, in shallow occasionally estuarine 
habitats. By contrast, the slightly less phyletically advanced 
members of Gnathopleustes are confined to open coast 
habitats of the North American Pacific region, but some 
(e.g., G. pachychaetus) exhibit brackish- water tolerance. 

Incisocalliope newportensis Barnard 
(Fig. 22) 

Incisocalliope newportensis Barnard, 1959: 22, pi. 2. 
Parapleustes pugettensis Barnard & Given, 1960: 43, fig. 
4.— Barnard, 1969b: 178.— Barnard & Karaman, 1991: 650. 

Material examined. J. L. Barnard's type specimen (Stn. 
#9, AHF- # 522) has been made available for this study, 
courtesy of the Los Angeles County Museum. 

Diagnosis. Female (5.0 mm): Head, eyes medium, oval, 
black. Antennae especially peduncles, stout. Antenna 1 the 
longer; peduncular segment 1 large, 2 & 3 short; flagellum 
long. Antenna 2, peduncular segment 5 > segment 4. 

Mandible, spine row with 8-9 blades; left lacinia 8-9 
dentate; palp segment 3 with 6-7 posterior marginal pectinate 
D spines. Maxilla 1, palp segment 2, surface setulose, 
segment 1 with single “shoulder” seta. Maxillas 2, inner 
plate broad, short. Maxilliped, inner plate with button 
spines. 

Coxal plate 1 large, expanding distally, little shorter 
than 2, with single postero-distal cusp. Coxa broad, width = 
depth. Gnathopods strongly subchelate, propods medium 
large; basis, anterior margin with a few scattered short setae; 
hind margin with a few setae proximally. Gnathopod 2, 
basis, anterior margin nearly bare. 

Peraeopods 3 & 4, segment 5 short, length < segment 5; 
Peraeopods 5-7, bases broad, convex behind; segment 5 
short dactyls strong. 

Pleon plate 3, hind comer acuminate, hind margin nearly 

straight. Uropod l,peduncle,outermargin strongly spinose. 


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96 


KEY TO SPECIES OF INCISOCALUOPE 


1. Coxa 1 distinctly shorter than coxa 2; gnathopod 1, basis, anterior margin strongly setose (20+ 

setae); peraeopods 3 & 4, basis, anterior margin lined with short setae throughout 2 

—Coxa 1 about as deep as coxa 2; gnathopod 1, basis, anterior margin nearly bare or with fewer 
than 15 setae; peraeopods 3 & 4 basis, anterior margin weakly setose 


2. Uropod 2, rami subequal; peraeopod 7, basis medium broad, postero-distal lobe ordinary, not 

reaching to segment 4; dactyls short, < 1/3 segment 6 L aestuarius (p. 104) 

— Uropod 2, outer ramus distinctly (1/3) the shorter; peraeopod 7, basis narrow, hind lobe deep, 
reaching segment 4 behind; dactyls heavy, strong, >1/3 segment 6 Lfilialis (p. 102) 


3. Gnathopods 1 & 2, propods relatively weak, depth not greater than carpus; gnathopod 1, basis 

with antero-distal cluster of 3 long setae 

—Gnathopods 1 & 2, propods relatively stout, strong, depth greater than carpus; gnathopod 1, bas- 
is antero-distally with 0-2, or 4, long setae 5. 


4. Gnathopod 2, basis with 2 strong antero-distal setae; antenna 1, peduncular segment 1 large, 

distinctly longer than segments 2 & 3 combined /• derzhavini (p. 102) 

Gnathopod 2, basis lacking strong antero-distal setae; antenna 1, peduncle 1 ordinary, length 

about equal to segments 2 & 3 combined nipponensis (p. 1(X)) 

5. Gnathopod 1, basis, anterior marginal setae long, length > width of basis; antenna 2, peduncular 

segment 5 not longer than 4 makiki (p. 98) 

Gnathopod 1, basis, anterior marginal setae short, length < width of basis; antenna 2, pedunc- 
ular segment 5, length distinctly > segment 4 6. 

6. Peraeopods 3 & 4, segment 5 regular, length ~ segment 4; antenna 2, peduncular segments 4 & 

5 slender, length 3-4 X width (p. 96) 

—Peraeopods 3 & 4, segment 5 short, thick, length < segment 4; antenna 2, peduncular segments 
4 & 5 relatively short, thick, length "'2X width 7. 


7. Peraeopod 4, coxa broad, width -depth; uropod 1, peduncular outer margin lined with 10-12 
strong spines; uropod 3, inner ramus with 5-6 pairs of marginal spines . . I. newportensis (p. 95) 
—Peraeopod 4, basis narrow, width < depth; uropod 1, peduncular margin proximally with cluster 
of 3-4 Stout spines; uropod 3, inner ramus, margins with 3-4 pairs of spines. /. dilatatus (p. 97) 


Uropod 2, outer ramus -3/4 inner ramus. Uropod 3, inner 
ramus with 6 pairs of marginal spines. Telson long, apex 
truncated. 

Taxonomic and distributional commentary. The 

type locality of Incisocalliope newportensis is Newport Bay , 
California. The species has been recorded authentically on 
the eastern Pacific coast only south of Pt. Conception. 1 1 
has been confused with Gnathopleustes pugettensis. How- 
ever, morphological differences are major, and the latter is 
also larger at maturity and more northerly in distribution. 

Incisocalliope newportensis and/, bairdi (J. L. Barnard) 
form a primitive species pair within the genus. Further 
species of the genus may yet be discovered, especially in the 
Baja and Gulf of California regions, and in the southern Sea 
of Japan and China Sea regions. Differences noted here 
between this pair and the remaining six species may eventually 
form a basis for recognition of the two phyletic groups at the 
subgeneric level (Fig. 43, p. 127). 


Incisocalliope bairdi (Boeck) 

(Fig. 23) 

Paramphitoe bairdi Boeck, 1871: 45-46, 50, pi. 1, fig. 3. — 
Barnard, 1956: 36, Plate 12. — Barnard & Karaman, 1991: 
650. 

Neopleustes bairdi Stebbing, 1906: 314-315. 

non Parapleustes pugettensis Barnard & Given, 1960. 

Diagnosis. Male (5.5 mm): Head, eyes medium large, 
oval-round, black. Antenna 1 the longer, flagellum 36- 
segmented. Antenna 2, peduncular segment 4 & 5 slender, 
segment 5> 4. 

Mandible, spine row with 1 5 blades; lacinia with 9 teeth; 
palp segment 3 with 9-10 posterior marginal “D” spines. 
Maxilla 1 , palp segment 2, apex with 7 spines and facial setal 
row, segment 1 with 2 short “shoulder “ setae. Maxilla 2, 
plates small, inner plate not broadened. Maxilliped, inner 
plate with 4-5 apicEil marginal “button” spines outer plate 
columnar; palp segment 3 large, heavy. 


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97 



FIG. 22. Incisocalliope newportensis (Barnard 1959). Female (5.0 mm). New port Bay, California. 


Coxal 1 large, broadening distally, lower margin gently 
convex, with single postero-distal cusp. Coxa 4 narrow, 
width < depth. Gnathopods large, strongly subchelate. 
Gnathopod 1, basis, anterior and posterior margins nearly 
smooth; merus with short distal process ; propod, hind margin 
straight, with single distal setal group. Gnathopod 2, hind 
margin of coxa with 2-3 short spines; basis nearly bare of 
setae. 

Peraeopods 3 & 4, segment 5 not shortened, length ~= 
segment 4. Peraeopods 5-7, bases medium broad, hind 
margins nearly straight; segment 5 not shortened. Dactyls 
medium. 

Pleon 3, hind comer acuminate, Uropod 1, peduncular 
outer margin with 7-8 spines, outer ramus very slightly the 
shorter. Uropod 2, outer ramus about 3/4 length of inner r am - 
us. Uropod 3, inner ramus with 5 pairs of marginal spines. 
Telson medium, narrowing to smoothly rounded apex. 

Taxonomic commentary. The species was first 
described by Boeck (1872) from southern California, and 


rediscovered in fresh material from the same region by J. L. 
Barnard (1956). Barnard's description and figures, more 
detailed than the accounts of Boeck (loc. cit.) and Stebbing 
“(1906) form the basis of the present analysis. 

Incisocalliope dilatatus (Ishimam) 

(Fig. 24) 

Parapleustes dilatatus Ishimam, 1984: 425, figs. 17-20.— 
Barnard & Karaman, 1991: 650.-Ishimam, 1994: 54. 

Diagnosis. Male (4.7 mm): Head, eye medium large 
almond-shaped, black. Antennae relatively short, first slightly 
the longer. Antenna 1, peduncular segment 1 short, thick; 
flagellum 27-segmented. Antenna 2, peduncular segments 4 
& 5 relatively long, slender, 5 > 4; flagellum 1 8-segmented. 

Mandible, spine row with 10 blades; left lacinia 9- 
dentate; palp segment 3 with 6 posterior marginal “D” 
spines. Maxilla l,palp segment 1 with 2 "shoulder” setae; 
segment 2, apex oblique, with 4 spines and numerous facial 



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98 



FIG. 23. Incisocalliope bairdi (Boeck, 1971). Male (5.5 mm). S. California, (after Barnard, 1956). 


setae. Maxilla 2, inner plate very slightly broadened. 
Maxilliped, inner plate with 3 apical “button” spines; outer 
pate, with 2 slender apical spines; palp segment 3 with distal 
inner facial scales . 

Coxal plate 1 large, distal margin convex, hind comer 
with 2 small cusps, posterior margin with 2 short spines. 
Coxa 4 medium, depth > width. Gnathopods strongly 
subchelate, propods relatively large. Gnathopod 1, basis 
with 1-2 stout anterior marginal setae, hind margin nearly 
bare; mems lacking postero-distal process; propod with 
superior medial facial cluster of setae; hind margin with 
single distal setal group. Gnathopod 2, anterior and posterior 
margins with weak, short setae; merus with strong postero- 
distal process. 

Peraeopod 3 & 4, segment 4 short, length > segment 5, 
dactyl medium. Peraeopods 5-7, bases broad, rounded 
behind; segment 5 short, length < segment 4. 

Pleon plate 3, hind corner acuminate. Uropod 1, 
peduncular outer margin relatively weakly spinose, with 
cluster of 3 strongest spines proximally; rami weakly 
marginally spinose; outer ramus distinctly the shorter. Uropod 
2, peduncle with 2 strong outer marginal spines. Uropod 3, 
rami short, inner ramus with 3-4 marginal spines. Telson 


relatively short narrowly slightly to broadly rounded apex. 
Female (6.0 mm). No discernible difference from the male 

Taxonomic commentary. Incisocalliope dilatatus is 
morphologically closest to /. makiki Barnard from the 
Hawaiian Islands (Fig. 44, p. 129). Both are members of 
the advanced subgroup that includes, /. derzhavini and I. 
filialis of the western Pacific region. 

Distribution. Japan Sea, southern shores of Hokkaido, 
under marine algae, LW level. Females ov. , May to August. 

Incisocalliope makiki (J. L. Barnard) 

(Fig. 25) 

Parapleustes derzhavini makiki Barnard, 1970: 227. 

Diagnosis. Female (4.2 mm): Head, eye medium large, 
reddish or dark brownish, irregularly roundish. Antenna 1 , 
peduncular segment 1 large > 2 & 3 combined, flagellum 24+ 
segmented. Antenna 2, peduncular segment 4 & 5 medium 
stout, subequal, flagellum 18+ segmented. 

Mandible, spine row with 8 blades, left lacinia 10-11- 


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99 



VIG.HX. IndsocamopedUatatus (Ishimaru, 1984). Male (4. 7 mm). Hokkaido, (after Ishimaru, 1984). 

dentate; palp segment 3, inner margin with 7 pectinate “D” 

setae. Maxilla 1, inner plate small, with 1 apical seta, 

Maxilliped, inner plate with 2 apical “button spines; outer 
plate with 2 slender apical spines; palp segment 3, with 
pectinations or scales at base of dactyl. 

Coxa 1 medium large, lower margin convex, hind comer 
with 1-2 cusps, hind margin with single spine. Coxa 2 with 
1 postero-distal cusp. Coxa 4 broad, as wide as deep. 

Gnathopods strongly subchelate; propod of gnathopod 2 

l3rger than 1. Gnathopod 1, basis, anterior margin with 


numerous (~10) strong setae, each longer than width of basis, 
hind margin weakly setose proximally ?; mems lacking distal 
process 1; propod with superior facial group of 2 setae; 
posterior margin bare. Gnathopod 2, basis virtually lacking 
marginal setae; merus with postero-distal process; propods, 
hind margin with distal group of spines and setae. 

Peraeopods 3 & 4, basis, margins weakly short-setose; 
segment 5 slightly shorter than 4; segment 6, hind margin 
spinose. Peraeopods 5-7, basis moderately broad, hind 
margins convex, lower hind lobe shallow, not reaching 


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100 



FIG. 25. Incisocalliope makiki (J. L. Barnard). Female (4.2 mm). Hawaii (after Barnard, 1970). 


segment 4; segment 5 shorter than segment 4. 

Pleon 3, hind comer minutely acuminate. Uropods 1 & 
2 strong. Uropod 1 , peduncle, outer margin strongly spinose; 
outer ramus distincdy the shorter. Uropod 3, inner ramus 
slender, margins with 6 spines. Telson short, broad, little 
longer than wide, normally rounding apically. 

Distribution. Oahu, Hawaiian Islands; 3-4 m in depth. 

Taxonomic commentary. Incisocalliope makiki merits 
full species status here. Its presumed common ancestor with 
I. dilatatus may have penetrated the Hawaiian archipelgo in 
the early Tertiary Period (p. 130). 


Incisocalliope nipponensisy new species 
(Fig. 26) 

Parapleustes denhavini Ishimaru, 1984: 417.-Ishimaru, 
1994: 54 (part.) 

Diagnosis. Female (5.0mm); Head, eye small, rounded, 
black. Antenna 1, peduncular segments 1-3 short, segment 
1 = 2 and 3 combined; flagellum, slender 25-segmented. 
Antenna 2, peduncular segment 4 shorter than 5, medium 
thick; flagellum slender, 24-segmented. 

Mandible, spine row with 8 blades; left lacinia 11- 
dentate; palp segment 3 with 7 posterior marginal “D” setae. 


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101 



FIG. 26. Incisocattiope nipponensis , new speci es. Female (4.6 mm). Japan Sea. (after Ishimaru, 1984). 

Maxilla 1, palp segment 1 with single “shoulder” seta; 
segment 2 apically with 4 spines and facial row of 3 setae. 

Maxilla 2, inner plate short, not broadened. Maxilliped, 
inner plate with 3 “button” spines; outer plate with 2 apical 
slender spines; palp segment 3 with distal inner marginal 
pectinations. 

Coxa 1 small, 1/3 shorter than 2, with single postero- 
dts^ cusp and 1 -2 posterior marginal short spines. Coxa 4 Type material Female “a” /5 n mmt c. 


Pleon plate 3, hind comer strongly acuminate. Uropod 

1, peduncle, outer margin strongly spinose, Uropod 2, inner 
ramus longer than peduncles, 1/3 longer than outer ramus. 
Uropod 3, inner ramus 1/3 longer than outer ramus, with 4- 
5 pairs of marginal spines. Telson medium long, narrowing 
to sharply rounded apex. 


weakly subchelate, propods only slightly broadened. 
Gnathopod 1, basis with 15+ long anterior marginal setae 
and ~ 10 short postero proximal marginal setae, merus with 
distal cusp; propod, hind margin with single distal spine. 
Gnathopod 2, basis, margins nearly bare merus with acute 
postero-distal cusp. 

Peraeopods 3 & 4, regular, segment 5 not noticeably 
shortened, dactyls medium. Peraeopods 5-7, base broadly 
expanded, hind margins convex, dactyls stout. 


2 females. Paratypes, at stations 2-4 along south coast of 
Hokkaido, 0.5 m depth, among algae. Collections of the 
Zoological Museum, Faculty of Science, Hokkaido 
University. 

Distribution. Shores of Hokkaido, LW to 5 m depth 
Sargassum belt, Laminaria belt; among Leathesia and other 
algae scraped from surface of boulders. 



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FIG. 27. Incisocalliope derzhavini (Gurj., 1938). Female (4.0 mm). Japan Sea. (after Gurjanova, 1951). 


Taxonomic commentary. This description is based on 
the careful work of Ishimaru (1984). He had previously 
found it very similar to the female (4.0 mm) of Neopleustes 
derzhavini from the sea of Japan, described by Guijanova 
(1951), that is treated below (see also Fig. 27). 


Incisocalliope derzhavini Gurjanova 
(Fig. 27) 

Neopleustes derzhavini Gurjanova, 1938: 317, fig. 31. 
Gurjanova, 1951: 645, fig. 442. 

Parapleustes derzhavini Barnard & Karaman, 1991: 650 
(part) 

Diagnosis. Female (4.0 mm): Head, eyes medium, 
round, black. Antenna 1, peduncle 1 large, length > seg- 
ments 2 & 3 combined; flagellum medium long, slender, 25- 
27 segmented. Antenna 2, peduncular segment 4 & 5 short, 
thick, 5 > 4; flagellum 18- segmented. 

Mandible, spine row with 6-8 blades; palp segment 3 
with 5-6 pectinate “D” spines. Maxilla 1, palp segment 1 
with 1 shoulder seta; segment 2, rounded apex with 4 spines. 
Maxilla 2, inner plate not broadened. Maxilliped, inner plate 
with 3 (?) button spines, palp segment 3 with pectinations at 
base of dactyl? 

Coxa 1 relatively short, little broadening distally, lower 
margin convex, with 1 hind cusp. Gnathopods relatively 


weakly subchelate; propods not deeper than respective carpus. 
Gnathopod 1, basis, anterior margin with 9-10 stout setae, 
concentrated distally, mostly longer than width of basis; 
merus lacking distal process; propod hind margin bare. 
Gnathopod 2, basis, antero-distal margin with 2 very large 
stout setae, hind margin nearly bare; merus with short distal 
process?, propod, hind margin with single distal seta. 

Peraeopods 3 & 4 ordinary. Peraeopods 5-7 ordinary; 
bases moderately expanded, ovate. 

Pleon plate 3, hind corner acuminate, lower margin 
gently convex, with 4-5 small spines. Uropod 3, inner ramus 
slender, margins each with 4 spines. Telson medium long, 
narrow, sharply rounding at apex. 

Distributional ecology. Japan Sea; tidal zone. 

Taxonomic commentary. Gurjanova's original figures 
and description are limited but sufficiently detailed to separate 
/. derzhavini from the material of Ishimaru (loc. cit.) des- 
cribed above as /. nipponensis, new species. 


Incisocalliope fHiaUs (Hirayama) 

(Fig. 28) 

Parapleustes filialis Hirayama, 1988; 40, figs. 265-268. — 
Barnard & Karaman, 1991: 650. — Ishimaru, 1994: 54. 


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FIG. 28. Incisocalliope filialiss (Hirayama). Male (3, 

Diagnosis. Male (3.5 mm): Body small, pleonites slightly 

raised postero-dorsally. Head, eyes medium large, nearly 
round, black. Antennae slender, medium long. Antenna 1, 
peduncular segment 2 short, - 1/2 segment 1 ; flagellum - 1 5- 
segmented. Antenna 2, peduncular segments 4 & 5 stout, 5 
slightly the longer; flagellum 16-segmented. 

Upper lip with relatively deep V-notch, lobes 
asymmetrical. Lower lip inner lobes broad, outer lobes 
oblique. Mandible, molar process small, vestigial; spine row 
with 6 short blades; incisor (left) with 4 proximal large teeth 
and 4-5 distal denticles; palp segment 3, basal “A” seta small, 
inner margin with 5-6 pectinate “D” spines; left lacinia 10- 
dentate. Maxilla 1, inner plate with single apical seta; palp 
segment 1 with single “shoulder” seta; distal segment, apex 
with 4-5 slender spines. Maxilla 2, inner plate short, not 
broadened, inner margin with single proximal plumose seta. 
Maxilliped, innerplate medium, inner margin notched distally, 
apex with 5 slender spines; outer plate slender, truncate apex 
with 2 slender spines; palp stout, segment 3 with distal 


5 mm). Ariake Sea, Japan, (after H irayama, 1988). 

pectinate denticles at base of dactyl; dactyl slender, straight, 

length about equal to segment 3. 

Coxal plates 1-3 lower margins broadly rounded, hind 
margins with 1 -2 median short spines, hind comers each with 
single cusp. Coxa 1 distinctly shorter than 2. Gnathopod 1, 
anterior margin of basis strongly setose, (20+ setae), some 
setae longer than width of basis; hind margin of basis 
proximally with 6-8 shorter setae.; carpus short, as deep as 
long, hind lobe stout; propod short, expanding distally, inner 
face with scattered setae; palmar margin convex, oblique 
slightly longer than hind margin, postero-distal angle with 
spine groups on either side of short dactyl-tip depression, 
distal spines larger; dactyl slender, with small distal unguis. 
Gnathopod 2, anterior margin of basis weakly setose, with 
single distal seta; hind margin proximally with row of setae; 
carpus short, hind lobe narrow propod subovate, longer and 
more slender than in gnathopod 1 ; two groups of longer and 
stronger spines at palmar angle. 

Peraeopods 3 & 4 relatively short and stout; bases. 



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FIG. 29. Incisocalliope aestuarius (Watting & Maurer, 1973). Female (4. 0 mm). Delaware Bay. 


anterior and posterior margins moderately strongly setose; 
segment 5 shorter than 4; segment 6, hind margin with 3 
groups of stout spines; dactyl heavy, medium. Peraeopods 
5-7, bases only moderately broadened, least in peraeopod 7, 
postero-distal lobes large, deep, reaching segment 4; segment 

5 shorter than 4; dactyls stout. 

Pleon plate 3, lower margin weakly spinose, hind corner 
squared, not acuminate. Pleopod peduncles, outer margin 
strongly setose. Uropods 1 & 2 large, extending well beyond 
uropod 3. Uropod 1, peduncle large, outer margin finely 
spinose. Uropod 2, outer ramus distinctly the shorter. Uro- 
pod 3, outer ramus long, length -2/3 long inner ramus, with 

6 pairs marginal spines. Telson oblong, apex subacute. 

Distribution. Ariake Sea, Japan; sublittoral. 

Taxonomic commentary. Hirayama likened Inch- 
calliope filialis to Incisocalliope derzJtavini but found sev- 
eral species differences. The species is an atypical Para- 
pleustes, with several features more reminiscent of Gnatho- 


pleustes. These include the unlike gnathopod propods, 

narrow peraeopod bases; and in mouthparts, the broad lower 
lips, "shoulder" seta on palp of maxilla 1, etc. The species is 
close to /. dilatatus in the armature of the maxilliped palp. 

Incisocalliope aestuarius (Watling & Mauer) 

(Fig. 29) 

Parapleustes aestuarius Watling & Mauer, 1973: 252, figs. 
1-4. — Fox & Bynum, 1975: 230. — Ishimaru, 1984: 431. — 
Barnard & Karaman, 1991: 650. 

Diagnosis. Female (4.0 mm): Head, eye small round, 
black. Antenna 1, peduncular segment 1 large, stout, length 
about equal to segments 2 & 3 combined. Flagellum long, 
-40 segments. Antenna 2, peduncular segments 4 & 5 short, 
medium, segment 5> 4; flagellum ! 25-segmented. 

Mandible, spine row with ~14 slender blades, distally 
largest; left lacinia 10-dentate; palp segment 3 with 8-9 
slender pectinate “D” spines. Maxilla 1, segment 1 with 


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105 


single shoulder seta; segment 2 , with numerous short facial 
seme, rounded apex with 4 spines; outer plate, inner apical 
spine elongate. Maxilla 2, inner plate not broadened. 
Maxilliped, inner plate with 2-3 apical marginal “button” 
spines; outer plate with 4 apical slender spines; palp segment 

3 distally with pectinations at base of dactyl. 

Coxal plate 1 short, lower margin convex, hind comer 
with 2-3 cusps posterior margin with 2-3 stout spines. Coxa 

4 little broadened deeper than wide. Coxa 5 deep. Gnathopods 
relatively weakly subchelate; basis, anterior margin lined 
with numerous (20+) setae some longer the width of basis, 
hind margin strongly lined with shorter setae; mems lacking 
distal cusp; propod relatively short, not deeper than carpus; 
with superior and inferior facial clusters of small setae; hind 
margin shorter than palm, with single distal setal group. 
Gnathopod 2, basis distal with short setae, hind margin 
distally with several setal groups; merus with short posterior 
tooth; propod, hind margin with 2 distal setal groups. 

Peraeopods 3 & 4 basis, anterior margin strongly short- 
setose; segment 5 shorter than 4; dactyls relatively short. 
Peraeopods 5-7, bases moderately broadened, hind margins 
convex; segment 5 slightly shorter than 4. 

Pleon plate 3, hind comer acuminate, slightly produced. 
Uropods 1 & 2 strong, rami longer than peduncle. Uropod 
1, peduncle, outer margin strongly spinose; rami subequal. 
Uropod 2 outer ramus little shorter than inner, margins 
strongly spinose. Uropod 3 rami long, slender, inner ramus 
with 7 pairs of margins spines. Telson medium long, apex 
rounded. 

Distributional ecology: From Delaware Bay, 
Chesapeake Bay to Albemarle Sound and estuaries of the 
southeastern states, on wharf pilings, among bryozoans, 
hydroids, and other sessile invertebrates. 

Taxonomic & distributional commentary. The 

original description (as Parapleustes aestuarius) is limited 
in a number of features, some of which were pointed out by 
Fox & Bynum (loc. cit.). The species is remarkably close 
morphologically to Incisocalliope filialis from the Sea of 
Japan. The relationship appears closely phyletic, but the 
disjunct distribution of the two forms defies explanation that 
is entirely satisfactory (see p. 130). 

Trachypleustes, new genus 

Type species. Trachypleustes vancouverensisy new species. 

Species composition. Trachypleustes trevori, new 
species (and varieties: Pribilof Islands, San Juan Batista I). 

Diagnosis. A group of small, smooth-bodied pleustids 
having short antenna 1 peduncular segments, unequal 
gnathopods, slender legs, slender unequal rami of uropods, 
and heavily chitinized, “molanzed”, or otherwise strongly 
modified mandibular blades. 


Body smooth above, slender. Head small; rostrum 
slightly produced beyond subacute head lobe. Eyes large. 
Antennae slender, elongate. Antenna 1, peduncle 1 large, 
without postero-distal process; segment 2 medium short; 
accessoiy flagellum minute, triangular, with a few apical 
setae. Antenna 2, peduncular segments 4 & 5 subequal, 
setose; flagellum elongate. 

Mouthparts strongly modified. Upper lip moderately 
incised and asymmetrical. Lower lip broad, squat, outer 
lobes oblique. Mandible, molar minute; spine row with few 
(4-6), strongly thicked and/or flattened blades; left lacinia 
irregularly 10-11 dentate; incisor multidentate; palp, segment 
3 longest, medial pectinate setae numerous ( 12+); segment 2 
sparsely setose medially. Maxilla 1, outer plate short, spines 
tall; palp long, apex with slender spines and setae, segment 
1 lacking lateral setae; inner plate 1-setose. Maxilla 2, inner 
plate medium broad, with 1 large inner plumose seta; 
maxilliped, palp and dactyl strong; inner plate short, apex 
sloping, with 3-5 button-teeth and 4-6 inner marginal setae; 
outer plate narrow, apex and inner margin slender-spinose. 

Coxal plates 1-4 increasing in size posteriorly; coxa 1 
small, not expanded distally; coxa 2-4 deeper than body 
plates; lower margins nearly straight, with hind cusp. 
Gnathopods 1 & 2 weakly subchelate, similar in form but 
unequal in size, not sexually dimorphic; gnathopod 2 distinctly 
the larger. Gnathopod 1, basis weakly setose anteriorly; 
carpus shallow, more than half length of propod; length of 
palm oblique, with small median tooth; length about equal to 
smooth hind margin; postero-distal angle with 2 groups of 
spines; dactyl slender. Gnathopod 2, carpus shorter, hind 
lobe deeper, anterior margin about half length of propod; 2- 
3 spine groups at posterior angle. 

Peraeopods 3-7 slender, dactyls normally developed. 
Peraeopods 5-7 normally homopodous; bases regularly broad 
and rounded behind; segment 4 (merus) postero-distal process 
strongly overhanging segment 5. 

Pleon plates 1-3 regular; lower margins spinose, hind 
comers variously acuminate. Pleopods strong, not sexually 
dimorphic. 

Urosome 2 not occluded dorsally. Uropods 1 & 2 
slender, marginally strongly spinose; rami unequal, inner 
ramus longer than peduncle. Uropod 3, rami markedly 
unequal, strongly spinose. Telson medium, apex rounded; 
penicillate setae slightly proximal to mid point. 

Coxal gills small to medium, saclike, largest on 
peraeopods 4 & 5. 

Distributional commentary. Members of the genus 
are known only from northern parts of the North American 
Pacific coastal marine region, in association with sponges 
and large sessile invertebrates. 

Etymology. A combining form of the Greek root 
''trachytes'^ roughness, and the generic name Pleustes, that 
alludes to the rough, molarlike appearance of the mandibular 
blades 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


106 


Taxonomic Commentary. This generic group is 
distinguished by the heavily molarized and pavementlike 
mandibular blades, the unequal, non sexually dimorphic 
gnathopods, slender peraeopods, and the elongate, spinose 
uropod rami. Phyletically the genus Trachypleustes appears 
closest to Gnathopleustes, but more distant from Inciso- 
calliope. 


Trachypleustes vancouverensis, new species 
(Fig. 30) 

Material examined. 
eBRITISH COLUMBIA. 

Northern Vancouver 1. : ELB Stn 0 1 , Cape Scott, Experiment 
Bight, under boulders, among algae, LW level, July 18, 
1959. - female ov. (4.5 mm), Holotype (slide mount), CMN 
Cat. no. NMCC 1995-0086. 

Diagnosis. Female ov. (4.5 mm): Head, rostrum pro- 
longed beyond lateral head lobe; eye subquadrate. Antenna 
1, peduncular segment 1 long, extending to midpoint of 
peduncular segment 4 of antenna 2; flagellum ~'28-segmented. 
Antenna 2, length about equal to antenna 1 ; flagellum -28- 
segmented. 

Lower lip, inner lobes very broad, shallow. Mandible, 
molar process prominent, apex blunt; spine row distally with 

4 thick short blades having rough, conical apices, and 
proximally with several short vestigial blades; cutting edge 
of incisor with 7-8 unequal teeth; palp segment 3 apex blunt, 
inner distal margin with 1 2 slender pectinate “D” spines; left 
lacinia large, broad, cutting edge with 10 small uneven teeth. 
Maxilla 1, palp slightly narrowing distally, rounded apex 
with 6 slender spines. Maxilla 2 outer plate narrow. Max- 
illiped, inner plate short, with 3 inner marginal plumose 
setae, and 4 apical button spines; outer plate slender, nar- 
rowly subtruncate, with 2 very slender spines; palp ordinary. 

Coxae relatively deep, broad, hind comers with single 
small cusp. Gnathopod 1, propod about half size of propod 
of gnathopod 2; palmar margin smoothly continuous with 
posterior margin; proximal spine group at postero-distal 
angle with single spine and split-tipped seta; posterior 
margin distally with single spine and setae. Gnathopod 2, 
carpal lobe, some distal setae pectinate; propod stout, 
subovate; proximal spine group at postero-distal angle with 

5 spines and split-tipped seta; posterior margin distally with 
small cluster of split-tipped setae. 

Peraeopods 3 & 4 ordinary, slender; segment 4, anterior 
margin with 3-5 tufts of slender spines; dactyls strong. 
Peraeopods 5-7 closely homopodous; bases broad, hind 
margins smoothly convex; margins of segments 4-6 with 
cluster of short spines; segment 5 slightly shorter than 4; 
dactyls strong, curved. 

Pleon plates 1-3, hind comers acuminate. Urosome 2 
with free dorsal margin. Uropod 3, outer ramus relatively 
long, -60% of inner ramus. 


Telson distally with several dorsal setules; apex unevenly 
rounded. Coxal gills on peraeopods 4-6 relatively large, 
broadly saclike. 

Etymology. The name alludes to the type locality on 
Vancouver Island, British Columbia. 

Distributional ecology. The species has been confirmed 
only for the type locality. Northern Vancouver Island, from 
under rock and algal habitats at LW level 

Taxonomic commentary. The species name vancouv- 
erensis alludes to its known distribution on Vancouver Is- 
land, British Columbia. 


Trachypleustes trevori, new species 
(Figs. 31, 32, 33) 

Material examined. About 130 specimens taken at 23 loc- 
alities, as follows: 

ALASKA. 

Pribilof Islands: D. B. Quayle coll., Nov. 23, 1965 - 1 female 
ov (slide mount). 

Southeastern Alaska. ELB Stns,. 1961: A168, Klokachef I - 
1 female; A175 , San Juan Batista L, under rock, among 
algae, LW level, July 26, 1961 - 1 female ov. (slide mount). 
BRITISH COLUMBIA. 

Queen Charlotte Islands; ELB Stn. E14a, Onward Pt. 
Moresby I. July 13, 1957 - 1 ov. female (slide mount), 2 other 
specimens. 

Northcentral coast. ELB Stns., July, 1964: H7, McCauley I. 

- 1 female ov; H65, Christie Pass - 2 females ov (slide 
mounts), 1 im. ELB , 1959, Stn. N22, off Banks 1. - 1 male 
(slide mount), 1 female, 28 other specimens. 

Northern Vancouver L: ELB Stns., July, 1959: V5, Lemon 
Pt., Nigei I. - 1 female ov (Slide mount); 03, Grant Bay - 5 
females ov (2 slide mounts). 

Southern Vancouver I.: ELB Stns., July 1970: P702 , Long 
Beach, south end, from algae and sessile invertebrates, 
under boulders, at LW level July 6-1 female; P719, 
Botanical Beach, from kelp and sponges, under boulders at 
LW level, Aug. 1-1 female ov. 

ELB Stns., 1975: P2, Bamfield Marine Laboratory, from 
floating log fouling community at surface, July 23-1 male, 

1 female, 2 im.; P5c, Taylor I., Trevor channel, from 
ascidians and sponges, under large boulder, July 25-2 males, 

2 females. 

ELB Stns., 1976 : B4, Off Brady’s Beach, naturalist's dredge, 
60-70 m, sand & algae June 25-1 female; B7, Wouwer I., 
Broken L, from algae and sponges on bedrock walls at LW, 
June 27 - 1 male, 1 female; B1 lb, Wickininnish Bay, south 
end, LW sandy mud, June 29-2 females; B28, Edward King 
L, among algae, under boulders, LW, July 10-1 female. 
ELB Stns., 1977: B13, Trevor Channel, off Brady’s Beach, 
6- 14m naturalist’s dredge, sand, stone, algae. May 25, 1977 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


107 



FIG. 30. Trachypleustes vancouverensis, n. sp. Female ov (4.5 mm). Cape Scott, Vancouver Island. 

^ Vancouver I.. LW level,Anita Voss coll., April 

NMCC1995-0084; 2 females, Paratypes, CMN Cat. No. 25, 1986 - 1 male (slide mount) + -40 other specimens 
NMCC1995-0085. B21b, Off Brady’s beach, 10-20 m O + 4U omer specimens. 

naturalist’s dredge, algae, debris over sand, June 1 - 3 fe- WASHINGTON-OREGON 

ofFnl'n ■ w ^ ^ ^August, 1966: W40, 

OffEdw^d King I., from sponge, W.C. Austin Stn. 101/76 Mukkaw Bay at Sooes Pt. - 2 females, 12 male (slide 

- 1 male (slide mount), 2 females. mounts); W58, Seal Rock - 1 male (slide mount). 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


108 



FIG. 31. Trachypleustes trevori, new species, 

Diagnosis. Female ov. (5.0 mm): Head, rostrum short, 
little exceeding lateral process; eye nearly round. Antenna 
1 much longer than antenna 2; peduncular segment 1 not 
exceptionally large, length slightly longer than segments 2 & 

3 combined; flagellum with ~42 segments, alternately with 
aesthetascs. Antenna 2, peduncular segments 4 & 5 relatively 
short, slender; flagellum with ~38 short segments, each with 
whorl of short setae. 


Female ov (5.0 mm). Trevor Channel, B. C. 

Lower lip, inner lobes relative narrow and deep. 

Mandible, molar minute much smaller than blades; spine 
row with 4-5 very short, thick, flat, pavementlike blades; 
cutting edge of incisor with 9-10 uneven teeth, smallest 
distally; palp segment 3 narrowing gradually, inner margin 
with 12 slender pectinate “D” spines; left lacinia broad, deep, 
cutting edge with 10 uneven teeth. Maxilla 1 palp cylindrical, 
obliquely rounded apex with 7 slender spines. Maxilla 2, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


109 




FIG. 32. Trachypleustes trevori, new species, A.-D locations; variations in mandibular blades & palp. 

outer plate regular. Maxilliped, inner plate with 6 inner 

marginal setae and 4 apical marginal “button” spines; outer 


plate, apex narrowly rounding, with singly slender spine; 
palp ordinary. 

Coxae 1-3 medium, relatively shallow, hind comers 
each with single small cusp. Gnathopod 1, propod much 
smaller than propod of gnathopod 2; proximal spine group at 
postero-distal angle with 2 spines; hind margin smooth, 
lacking spines or setae. Gnathopod 2, carpal lobe lacking 
pectinate setae; propod with proximal group of four spines at 
postero-distal angle; hind margin with distal cluster of short 
simple setae. 


Peraeopods 3 & 4 ordinary, slender; segment 4, anterior 
margin weakly setose; dactyls medium. Peraeopods 5-7, 
bases not exceptionally broad, increasing posteriorly; 
segments 4-6, margins with clusters of short spines; segment 
5 not shorter than 4; dactyls medium, curved. 

Pleon plates 1 & 2, hind comers acuminate; pleon plate 
3, hind comer squarish. Urosome 2, dorsal margin nearly 
occluded by segments 1 & 3. Uropods 1 & 2 long, slender, 
margins of rami strongly serially spinose. Uropod 3, outer 
ramus short, length -1/2 slender inner ramus having 7-8 
pairs of marginal spines. 


AMPHIPACIFICA VOLE NO. 1. AUG. 31, 1995 


110 



A 

Pribilof i. 
Female (4,0 mm) 


B 

Experiment Cove 
Female (4.5 mm) 


off Brady's beach 
Female (5.0 mm) 


off Brady's Beach 
Female (5.0 mm) 


FIG. 33. Trachypleustes trevori, new species. A-E locations. Variations in mandibular blades & palp. 


Telson ordinary, apex smoothly rounded. Coxal gills on 
peraeopods 4-5 short, saclike 

Etymology. The species name alludes to the type locality 
in Trevor Channel, Vancouver Island, British Columbia. 

Distributional ecology. The species ranges from 
southeastern Alaska, commonly throughout British Columbia 
to central Oregon, along exposed rocky coasts, associated 
with sponges and tunicate in under-rock habitats at LW level . 


Taxonomic commentary. Material from the following 
stations are presently considered variants ofT. trevori . This 
treatment is not entirely satisfactory, since "variants" may 
prove to be specifically distinct when more extensive material 
can be studied: 

Trachypleustes (small-eyed variety, Fig. 32D) having only 
3-4 “pavement blades”, at Stns. A175; H14a: W40; W58. 
Trachypleustes (northern variety, Fig. 33 A) having 5-6 
thick, acute blades, palp with 6-7 pectinate spines, from the 
Pribilof Islands, Bering Sea. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 
Micropleustes, new genus 


111 


Parapleustes Barnard, 1969a: 425 (partim). — Ishimam, 1984: 
432 (partim). — Barnard & Karaman, 1991: 649 (part). 

Type species. Parapleustes nautilus J. L. Barnard 1969b: 
199. 

Species composition. Micropleustes behningi (Ishi- 
maru, 1984); M. behningioides, new species; M. longimanus 
(Ishimam, 1984); M nautiloides, new species. 

Diagnosis. Body small, smooth to slightly mgose above. 
Head, rostmm very short; head lobe subacute; inferior antennal 
sinus elongate, shallow. Eyes small, roundish. Antennae 
short, subequal, flagellaUttlelonger than respective peduncles, 
weakly setose; accessory flagellum minute. Antenna 1 shghtly 
the longer in male. 

Mouthparts somewhat modified. Upper lip shallowly 
and submedially notched, lobes slightly asymmetrical. Lower 
lip wide, inner lobes deep, outer lobes oblique, rounded. 
Mandible: incisor with few (6-8) teeth; left lacinia 6-9 
cuspate; blades medium heavy, distally pectinate, 7-9 in 
number; molar small, apex blunt, weakly setulose; palp seg- 
ments relatively short, stout; segment 2 with few (3-8) inner 
marginal setae; segment 3 subequal with few (5-10) inner 
marginal pectinate setae. Maxilla 1, outer plate with 9 tall 
apical spine-teeth; inner plate with single apical setae, 
occasionally lacking; palp segment 2 normal, apex with 4 
short spines, segment 1 with 1+ outer marginal setae. Maxilla 
2, inner lobe slightly broadened, inner margin often with 2 
plumose setae. Maxilliped, segment 3 not conspicuously en- 
larged, longer than palp segment 1; dactyl strong, palp 
segment 3 lacking distal process; inner plate with 1-2 stout, 
apically pectinate inner marginal setae. 

Coxal plates large, broad, deep; coxa 1 not broadened 
or bent forward distally; postero-distal notch minute, often 
multiple (2-4). Gnathopods small to medium strong, not 
sexually dimorphic; propod tending to elongation; carpus 
variable, hind lobe short or lacking; palm of propod shorter 
than posterior margin, smoothly convex, lacking median 
tooth, postero-distal angle with 1-2 groups of spines. 

Peraeopods 3-7 short, medium stout, normally spinose; 
segment 5 distinctly shorter than 4; dactyls normal, strong. 
Peraeopods 5-7 regularly homopodous, bases very broad. 

Pleon side plates deep, medium broad, hind comers little 
produced. Pleopods normal, not sexually dimorphic, rami 
subequal, slightly longer than peduncles. Urosome short, 
segment 2 nearly occluded dorsally. Uropods short; rami of 
uropod 1 and uropod 2 subequal, outer slightly the shorter, 
sparsely spinose, about equal in length to peduncle. Uropod 
3 short, extending less than twice length of telson; outer 
ramus distinctly the shorter. 

Telson elongate, dorso-lateral penicillate setae mark- 
edly distal. Coxal gills of two types: anterior two pairs 
slender, sublinear; posterior three pairs larger, platelike, 
smallest on peraeopod 6. 


Etymology. A combining form of the Greek “mikros “ 
(small) and the root generic name “pleustes”, referring to the 
small body size of component members of the genus. 

Distributional ecology. All five species of the genus are 
endemic to the North Pacific region, three on the Asiatic, and 
two on the North American coast. 

Taxonomic commentary. Within subfamily Parapleust- 
inae, the genus Micropleustes occupies a somewhat isolated 
position. It combines a number of relatively plesio-morphic 
character states, especially in the mouthparts, with arelati vely 
advanced condition of the antennae, coxal plates, gills, 
uropods, and telson. In balance, however, the genus is least 
distant from the type genus Parapleustes (p. 127). 

Micropleustes nautilus (J. L. Barnard) 

(Fig. 34) 

Parapleustes nautilus J. L. Barnard, 1969b: 199, fig. 55. — 
Austin, 1985: 592.— Staude, 1987: 379, fig. 18.77.— Barnard 
& Karaman, 1991: 650. 

Material examined. About 185 specimens in 44 lots: 
ALASKA. 

Bering Sea: Attu I., Massacre Bay, C. E. O’Clair coll, June 
23, 1972 - 2 females. 

Amchitka I., Banjo Pt., Sta. BlGl, C. E. O’Clair coll. Aug. 
14, 1971 - 32 specimens incl. males, females, im. (male, 
female slide mounts); Ibid.. Stn. IA-2, plot 28, bedrock reefs 
uplifted by underground nuclear tests. May 22, 1974 - 2 
females. 

Southeastern Alaska. ELB Stn. S5B7, 1980 - 1 female. 
BRITISH COLUMBIA. 

Queen Charlotte Islands. ELB Stns., June- July, 1957: W4a 
(1);W12(1); W9a(l);H14(l). 

Northcentralcoast. ELB Stns., July, 1964, 1959: H1(4);H33 
(8); H39 (2); H44 (-20); H47 (1); N1 (1). 

Vancouver I., north end. ELB Stns, July, 1959: 01 (4); 05 

(1) ;07b (4); 015 (1). 

Vancouver I., southern end. ELB Stns., July-August, 1955: 
FI (2);P4(l);P6c(3). 

ELB Stns., 1970: P702 (2); P712 (7). ELB Stns., 1975: P3a 

(2) ; P5a (2); P5b (2); P5d (3); P20 (2). ELB Stns., 1976: B3 
(l);B13(5);B28(2).ELBStns.,1977:B6a(l);B8(2);Bllb 
(l);B19b(2). 

Wizard Inlet, D. Kittle Stn. 712, July 28, 1972 - 1 male, 1 
female (fig'd specimen) (slide mounts) -i- 1 female, 3 im. 
Barkley Sound, Broken I. group, C. Lobban coll., July 7, 
1971 - 1 female; Ibid.. July 9-10 specimens. Bordelais I., 
from sponge at LW level, R. J. Anderson coll, June 26, 1976 
- 1 male (slide mount). 

WASHINGTON-OREGON. 

Coastal localities. ELB Stns., July-August, 1966: W22 (1); 

W40 (8); W58 (-15 ); W60 (6). 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


112 



FIG. 34. Micropleustes nautilus (J. L. Barnard). Female ov (3.1 mm). Wizard Inlet, B. C. 


AMPfflPACIFICA VOL II NO. 1. AUG. 31, 1995 


113 


KEY TO SPECIES OF MICROPLEVSTES OF THE NORTH PACIFIC REGION 


1. Gnathopods, propod elongate, length of lower margin -2Xpropod depth; palm of propod short, length 
less than half that of posterior margin; maxilla 1 , inner plate bare; inner ramus of uropods 1 shorter than 
peduncle 2 

—Gnathopods, propod not elongate, length less than twice depth; propod palm normal, length more than 

half postenor margin, maxilla 1 inner plate with single apical seta; uropods 1, inner ramus not shorter 
than peduncle ,, 


2. Gnathopod 1, carpus distinctly longer than carpus of gnathopod 2; coxal plates 1-4 only slightly deeper 

than corresponding body plates; peraeopods 5-7, segment 4 wide, width = length; telson length about 
twice width, hnguiform in shape m. longimanus (p. 1 17) 

—Gnathopod 1, carpus about equal to that of gnathopod 2; coxal plates 1-4 very deep, much deeper than 
corresponding body plates; peraeopods 5-7, segment 4 normal, length distinctly greater than width; tel- 
son length about 3 X width, apex narrowly rounding m. nautiloides, n. sp. (p. 1 13) 

3. Peraeopod 7, segment 4 postero-distally nearly totally overhanging segment 5 ... M, behningi (p. 1 15) 

Peraeopod 7, segment 4 less broad, postero-distally overhanging segment 5 by 1/2 to 2/3 4. 

4. Gnathopods, palm of propod distinctly shorter than posterior margin; postero-distal palmar angles with 

two distinct groups of spines; telson regularly narrowing distally M. nautilus (p.l 1 1) 

—Gnathopods, palm of propod about equal in length to posterior margin, postero-distal angle with two 
tight clusters of spines appearing almost as one group; telson, margins constricted medially 

behningioides (p. 116) 


Coos Bay, Oregon, K. E. Conlan Stn. 08-23 - 2 females, 8 
other specimens. 

Diagnosis. Female ov (3.2 mm): Body and coxal plates 
medium deep. Head, eye round, black. Antenna 1 medium, 
peduncle 1 large, length> segments 2 & 3 combined; flagellum 
14-segmented. Antenna 2, slightly longer than 1, peduncular 
segment 4 & 5 subequal; flagellum 14-segmented. 

Upper lip with broad apical V-cleft; lobes asymmetrical. 
Lower lip, inner lobes shallow, outer lobes smoothly ovate, 
oblique. Mandible, molar very small apex rounded; spine 
row with 7-9 medium, distally pectinate blades; cutting edge 
of incisor with 7-8 unequal teeth; palp segment 3 with 9 inner 
marginal pectinate spines and 1 long terminal seta; left 
lacinia 8-dentate. Maxilla 1, inner plate with single apical 
seta, palp segment 1 with single “shoulder” seta; segment 2 
slightly broadest medially, apex with 4 spines. Maxilla 2, 
inner plate slightly broadened distally, inner margin with 2 
plumose setae. Maxilliped, inner plate with 2 inner marginal 
spines and 2 apical teeth; outer plate medium, narrowing to 
rounded apex, with 2 slender curved spines; palp, dactyl 
slender minutely pectinate, not longer than segment 3. 

Coxa 1 broadest distally. Coxa 5, lobes shallow. 
Gnathopod 1, carpus short, deeper than long; propod short- 
rectangular, length -1 .5 X depth, with proximal cluster of 2 
stout median facial setae; palmar margin short, convex, 
postero-distal angle with cluster of 5 spines; hind margin 
nearly straight, with distal cluster of 2 spines; dactyl weakly 
setulose behind. Gnathopod 2 subsimilar, propod slightly 
heavier and deeper than in gnathopod 1. 

Peraeopods 3 & 4 relatively short and stout, segment 4 
slightly broadened; dactyls short. Peraeopods 5-7 closely 


homopodous in size and form; bases broad, rounded behind, 
postero-distal lobe medium deep; segment 4 slender, postero- 
distal lobe overhanging segment 5 by half its length; dactyls 
medium, length about 1/2 segment 6. 

Pleon plate 3, hind comer not acuminate. Uropodl slen- 
der, rami subequal, with 1 -2 marginal spines. Uropod 2, rami 
subequal, slightly shorter than peduncle. Uropod 3, outer 
ramus short, with 3-4 marginal spines, length - 1 .5 X each of 
peduncle and outer ramus. 

Telson medium, slightly narrowing distally to rounded 
apex, penicillate setae distal. 

Distribution. From SE Alaska to middle and southern 
California, intertidal to shallow depths (5 m), associated 
with under-rock algal and sponge communities. 

Taxonomic commentary. Morphological variations 
were noted in O’Clair material from Alaska, and in ELB 
material at Stns. F*7 1 2 and W40, but were not considered sig- 
nificant at the species level. 


Micropleustes nautiloides, new species 
(Fig. 35) 

Parapleustes species "A" J. L. Barnard, 1969b: 203? 

Material examined: 

BRITISH COLUMBIA. 

Southern Vancouver!.: ELB Stn. P712, Off Hanes L, Trevor 
Channel, under boulders and algal mats, LW level, July 2 1 , 
1970 - 4 males, 2 females, 2 im. 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


114 



FIG. 35. Micropleustes nautiloides, new species. Female ov (2.9 mm). Sunset Bay, Oregon. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


115 


WASHINGTON-OREGON. 

Coastal Localities. ELB Stn. W40, Mukkaw Bay, at Sooes 
Pt., from bedrock walls and under boulders, LW level, July 
31, 1966 - 9 specimens. Sunset Bay, south of Charleston, 
Coos Co., K. E. Conlan Stn. 06-06, in Rhodomela larix^ July 
8, 1986 - female (2.9 mm) Holotype (slide mount), CMN 
Cat. no. NMCC 1995-0074; Ibid.. Stn. 06-03 - 3 females (to 
3.1 mm) (1 slide mount), Paratypes, CMN cat. No. 
NMCC 1995-0075; Ibid.. Stn. 06-12 - 9 females ov, 3 imm; 
Ibid. . Stn 08-6 - 2 im. 

Diagnosis. Female ov (2.9 mm): Body and coxal plates 
deep. Head small, flat-rounded, black. Antennae short. 
Antenna 1, peduncular segment 1, length = segments 2 & 3 
combined; flagellum 11 -segmented. Antenna 2, slender, 
slightly the longer, flagellum 1 1 -segmented. 

Upper lip deep, with narrow apical V-notch; lobes 
nearly symmetrical. Lower lip inner lobes deep, outer lobes 
large, oblique. Mandible, molar medium, apex sharply 
rounded; spine row with 7-9 stout distally pectinate blades; 
cutting edge of incisor with 7 unequal teeth; palp segment 3 
with elongate basal “A” seta, inner margin with 9 pectinate 
spines; left lacinia 8-dentate. Maxilla 1, inner plate small, 
lacking apical set; palp segment 1 with single “shoulder seta; 
palp segment , narrowing, with 4 apical spines. Maxilla 2, 
inner plate broad, with 2 inner marginal plumose setae, 
maxilliped inner plate large, narrowing distal with 2 inner 
marginal spines, and 3 apical marginal short spines; outer 
plate relatively tall, with single curved spine at subconical 
apex; dactyl nearly straight, minutely pectinate, not longer 
than segment 3. 

Coxal 1 little expanded distally, hindcorner with 3 small 
cusps. Coxae 2-3, depth ~2X width, hind comers each with 
3 small cusps. Coxa 4, width = depth. Coxa 5 , lobes deep. 
Gnathopod 1, carpus longer than deep, hind lobe shallow, 
short; propod slender, elongate, length ~2X depth, palmar 
margin short, oblique convex, postero-distal angle with 
group of 4-5 spines, one distinctly largest; hind margin 
straight, with distal cluster of 2 short spine and a few cleft- 
tipped setae; dactyl short, weakly setulose behind. Gnathopod 
2 closely subsimilar, propod slightly stouter. 

Peraeopods 3 & 4, slender; dactyls medium. Peraeopods 
5-7 homopodous; segment 4 relatively short, broad, postero- 
distal process overhanging 2/3 of short segment 5; dactyls 
large, length > 1/2 segment 6. Peraeopod 5 slightly shortest; 
basis broadest, rounded behind; bases of peraeopods 6 & 7 
less expanded, hind margin nearly straight. 

Pleon plate 3, lower margin convex, hind comer acute, 
produced. Uropods 1 & 2 rami shorter than peduncle, 
distally narrowing. Uropod 2, outer ramus distinctly the 
shorter. Uropod 3 ordinary, inner ramus with 3 marginal 
spines. Telson elongate linguiform, narrowing to sharply 
rounded apex; penicillate setae distal. 

Distributional ecology. From central British Columbia 
to southern Oregon, possibly central California, intertidally 
and inimediately subtidal, in algal mats (Rhodomela) and 


Phyllospadix clumps, of lotic high salinity waters. 

Etymology. A combining form of “nautilus” + “oides” 
in reference to the overall similarity of this species to 
Micropleustes nautilus. 

Taxonomic commentary. Micropleustes nautiloides 
is taxonomically closer to M. longimanus than to M. nautilus 
(see Fig. 38, p. 118). Parapleustes sp. "A*' of Barnard 
(1969b) may be this species. 

Micropleustes behningi (Guijanova) 

(Fig. 36) 

Neopleustes behningi Gurjanova, 1938; 315, fig. 30. 
Pleustes behningi Guijanova, 1951: 641, fig. 438. 
Parapleustes behningi Barnard & Karaman, 1991: 650 
(part). — Ishimaru, 1994: 54 (part?). 

Parapleustes behningi Ishimam, 1984: 407, figs. 3-9. 

Diagnosis, (mainly after Gurjanova, 1951). Female (1.5 
mm): Body and coxal plates short, deep. Head, eye 
subquadrate, black. Antennae very short. Antenna 1 , ped- 
uncular segment 1 stout, length ~ 2X segments 2 & 3 com- 
bined; flagellum 8-segmented. Antenna 2 stout, slightly the 
longer; peduncular segment 4 & 5 very short; flagellum 8- 
segmented. 

Upper lip with narrow epistome; labrum, lobes nearly 
symmetrical. Lower lip broad, shallow, outer lobes ovate, 
nearly vertical. Mandible, molar short, apex bluntly rounded; 
spine row with 7-8 uneven blades, distally thick, proximally 
short, slender; cutting edge of incisor with 6(?) irregular 
teeth; left lacinia 7-8 dentate. Maxilla 1, inner plate small, 
with short apical seta; palp slender, segment 1 lacking 
shoulder seta; segment 2 slender, with 3? apical spines. 
Maxilla 2, inner plate small, little broadened distally, with 
single short inner margin plumose seta Maxilliped, inner 
plate regular; outer plate short, with 2 curved spines at round- 
ed apex; palp, dactyl stout, slightly longer than segment 3. 

Coxae 1-4 relatively deep, narrow. Coxa 1 not expanded 
distally, hind Comer with single stout cusp. Coxa 2, distal 
margin straight, hind comer with 4-5 distinct cusps. Coxa 4 
deeper than broad. Gnathopod 1, carpus short, depth > 
length; propod medium long, length -1.5 X depth, palmar 
margin short, oblique, nearly straight; postero-distal angle 
with cluster of 3 stout spines; hind margin straight, with 
distal spine; dactyl strong, minutely setulose behind. 
Gnathopod 2, somewhat similar, but carpus slightly shorter, 
hind lobe deeper and narrower than in gnathopod 1; propod 
more elongate and more slender; length - 2X depth. 

Peraeopods 3 & 4 slender, margins of segments 4-6 
weakly spinose; dactyl strong, > 1/2 segment 6. Peraeopods 
5-7 relatively short; bases medium broad, hind margin convex, 
with 6-8 broad crenulations; segment 4 short, postero-distal 
process elongate, nearly totally overhanging short segment 
5 by 80%; dactyls large. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


116 



FIG. 36. Micropleustes behningi (Gurjanova). Female (4.0 mm). Japan Sea. (after Gurjanova, 1951). 


Micropleustes behningioides, new species 
(Fig. 37) 

Parapleustes behningi Ishimaru, 1984: 407, fig. 4. — Barnard 
& Karaman, 1991; 650 (part). — Ishimaru, 1994: 54. 

Diagnosis. Female (5.9 mm). Body short, compact, 
coxal plates deep. Head, eye round, medium large. Antenna 
1, peduncular segment 1 short < 2 & 3 combined; flagellum 
long, relatively stout, 19-segmented. Antenna 2 shorter, 
peduncular segments 4 & 5 short, subequal; flagellum 16- 
segmented. 

Upper lip regular, lobes slightly asymmetrical. Lower 
lip inner lobes, deep, outer lobes large, oblique. Mandible, 
molar prominent, slender, apex subacute; spine row with 9 
short stout blades; cutting edge of incisor with 8 unequal 
teeth; palp segment 3 with short, proximal "A" seta, and 10? 
inner marginal pectinate “D” spines; left lacinia with 7(?) 
teeth. Maxilla 1, inner plate with single apical plumose seta; 
palp segment 1 with 2 "shoulder" setae; segment 2, surface 
finely setulose, apically with 4-5 short spines. Maxilla 2, 
inner plate short, broadly expanded, inner margin with 2 
unequal plumose setae. Maxilliped, inner plate medium, 
with few distal facial setae, and 4 apical marginal spines; 
outer plate short, apex narrowly rounded, with 2 slender 
spines; palp, dactyl stout, nearly straight, not longer than 
segment 3. 


Coxa 1-3 medium broad, deep. Coxa 1 slightly broadened 
distally, hind comer with 1-2 minute cusps. Coxae 2 & 3, 
hind comer with 3 minute cusps. Coxa 4 deeper than broad. 
Coxa 5 lobes deep. Gnathopod 1, carpus short, deep, hind 
lobe narrow; propod short, length ~1.5X width; palmar 
margin relatively long, about equal to posterior margin, 
convex, oblique, postero-distal angle with 3 spines; dactyl 
minutely setulose behind. Gnathopod 2 subsimilar; carpus 
slightly shorter and deeper; propod slightly expanding distally . 

Peraeopods 3 & 4 stout, 3 distinctly the larger; segment 
4 broadened abmptly, with subparallel margins; dactyls 
medium strong. Peraeopods 5-7 short, subsimilar; bases 
moderately expanded, hind margins gently convex, minutely 
crenulate; hind lobes deep; segment 4 broadened, nearly as 
wide as deep, postero-distal lobe 2/3 overhanging short 
segment 5; dactyls stout. 

Pleon plate 2 , hind comer rounded; pleon plate 3 hind 
comer acuminate. Uropods 1 & 2 short, little or not exceeding 
uropod 3. Uropod 1, rami and peduncle subequal in length. 
Uropod2, outerramus distinctly the shorter. Uropod 3, outer 
ramus shorter, length barely 1/ inner ramus. 

Telson slender, “pinched” medially, narrowing to 
rounded apex; penicillate setae distal. 

Etymology. A combining form of the species name 
“behningi “ and the suffix "oides ", like the regionally co- 
occurring species M. behningi (Gurjanova, 1938). 


AMPHIPACIFICA VOL 11 NO. 1. AUG. 31, 1995 


117 



Type material. Ishimam, 1984, figs. 3-7: Female "a" 
(5.9 mm), Holotype, Samani, Hokkaido; Ibid-, fig. 8: Male 
"e" (4.0 mm), AUotype, Oshoro, Hokkaido. Collections of 
the Faculty of Science, Hokkaido University. 

Distribution. Eastern Sea of Japan and southern Hok- 
kaido, among andSargos^w/n, LW-0.5 m depth. 

Taxonomiccommentaiy. Micropleustes behningioides 
is readily separable from M. behningi (Guijanova, 1938), 
and appears morphologically closer to M. nautilus (see key,’ 

p. 113; also fig. 34, p. 112 ). 


Parapleustes longimanus Ishimam, 1984: 438, figs. 25-28. 
—Barnard & Karaman, 1991: 650.— Ishimam, 1994: 54. 

Diagnosis. Female (2. 9 mm); Body short, compact, 
coxal plates medium deep. Antennae short, slender, subequal. 
Antenna 1, peduncular segment 1 short, length < segments 
2 & 3 combined; accessory flagellum broadly conical, with 
4 apical setae; flageUum 8-segmented. Antenna 2, peduncular 
segments 4 & 5 slender, subequal; flagellum 8-segmented. 

Upper lip shallowly V-cleft apically, lobes nearly 
symmetrical. Lower lip, inner lobes deep, outer lobes small 
ovate, oblique. Mandible, molar process, short, conical; 


AMPHIPACMCA VOL II NO. 1. AUG. 31, 1995 


118 



FIG. 38. Micropleustes longimanus (Ishimaru). Female (2.9 mm). Japan, (after Ishimaru, 1984). 


spine row with 6-7 short blades; cutting edge of incisor with 
6-7 unequal teeth; palp segment 3 with 5 inner marginal 
pectinate “D" spines; left lacinia 6-7-dentate. Maxilla 1, 
inner plate small, lacking apical seta; palp segment 1 lacking 
“shoulder” seta; segment 2 narrowing distally, apex with 3- 
4 slender spines. Maxilla 2, inner plate slightly shorter than 
outer plate, little broadened, with 1 short inner marginal 
plumose seta. Maxilliped, inner plate very short, with 1 inner 


marginal stout seta, apex with 2 stout and 2 slender spines; 
outer plate very short, subtruncate apex with 2 slender 
spines; palp, dactyl curved shorter than segment 3. 

Coxae 1-4, lower margins rounded. Coxa 1 slender, 
hind comer with single small cusp. Coxae 2-3, lower border 
minutely crenulate, hind comer with single cusp. Coxa 4 
deeper than wide. Coxa 5, lobes deep. Gnathopodl, carpus 
slender, hind lobe very small, length ~2X depth; propods 



AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


119 


slender, length ~3X depth, margins subparallel, palmar margin 
very oblique, very short, postero-distal angle with single 
cluster of 3 spines (one large); dactyl short, inner margin with 
5 short curved setules. Gnathopod 2 subsimilar, except 
carpus and propod slightly shorter and deeper. 

Peraeopods 3 & 4, segments 4-6 relatively stout, 4 not 
broadened; dactyl medium. Peraeopods 5-7 very short, closely 
subsimilar; bases broad, lower hind lobes very deep, hind 
margins gently convex; segment 4 expanded, broader than 
deep, postero-distal lobe nearly totally overhanging short 
segment 5; segment 6 stout, with 2 anterior marginal spines; 
dactyl medium. 

Pleon plate 3, hind comer squared. Pleopods, peduncles 
stout, outer margins short-spinose; rami short, 12-segmented. 
Uropods 1 & 2 slightly exceeding uropod 3. Uropod 1 , rami 
subequal weakly marginally spinose. Uropod 2, outerramus 
slightly the shorter. Uropod 3, outer ramus short, length 
-60% inner ramus. Telson short, slightly narrowing distally 
to broadly rounded apex; penicillate setae marginally 
subapical. 

Distribution. The species is known from inshore 
shallows of the mainland and Japanese coast of the Sea of 
Japan. 

Taxonomic commentary. Micropleustes longimanus 
is distinctive in nearly every character state, but in balance 
appears closest to Af. nautiloides ofthe North American Pac- 
ific region. 

Dactylopleustinae, Bousfield & Hendrycks 

Dactylopleustinae Bousfield & Hendrycks, 1994: 38. 

Type Genus. Dactylopleustes Karaman & Barnard, 1979, 
monotypy. 

Diagnosis. A monotypic group of primitive but second- 
arily specialized commensal and/or parasitic pleustids. 

Rostmm short. Eyes large, reniform. Antennae short, 
pediform. Accessory flagellum minute. 

Upper lip, notch shallow, lobes only slightly asymmetri- 
cal. Lower lip with deep, distinct inner lobes. Mandible, 
molar rounded, non-triurating; palp segment 2 short, seg- 
ment 3 swollen, lacking baso-facial CA") setae ; right lacinia 
lacking; Maxilla 1, outer plate short, wide, with 9-16 
pectinate spine-teeth; inner plate with 1 apical seta; palp 
large, terminal segment broad. Maxilla 2, plates short, 
subequal. Maxilliped, plates small, weakly armed; palp 
segments short; dactyl pectinate. 

Coxae 1-4 deep, 1 shortest. Gnathopods with elongate 
carpus and propod, longer in gnathopod 2; palmar margins 
short, lacking median tooth, hind margin setose. 

Peraeopods 3-7 short; dactyls short, inner margins finely 
crenulate or pectinate. Peraeopods 5-7 basically homopodous; 
coxae regularly and strongly postero-lobate; bases broad. 

Pleon plates regular, unmodified. Urosome 2 not oc- 


cluded dorsally. Uropods 1 & 2 broad-lanceolate, rami sub- 
equal, broad-lanceolate. Uropod 3 medium, rami unequal. 
Telson keel proximally. 

Coxal gills saclike on peraeopods 2-4, plate-like on 5 

& 6 . 

Taxonomic commentary. This monotypic group (con- 
sisting to date of three species in one genus) was formerly 
assigned to the genus Parapleustes based on the non-triturat- 
ing molar and ordinary form of the maxillipedal palp. How- 
ever, the unusual mixture of plesiomorphic and apomorphic 
character states justified elevation of the genus Dactylople- 
ustes to subfamily ranking (Bousfield & Hendrycks, 1994). 

Dactylopleustes Karaman & Barnard 

Parapleustes Tzvetkova 1975: 121 (part). 

Dactylopleustes Karaman & Barnard, 1979: 112.— Barnard 
& Karaman, 1991: 647. 

Type species. Parapleustes echinoicus Tzvetkova, 1975, 
original designation 

Species,Dactylopl€ustesechinoides, new species (p. 121); 
D. (Apodactylopleustes) obsolescens Hirayama, 1988. 

Diagnosis. Body small, smooth above, lysianassiform; 
coxae deep, legs short. Head, rostrum short, about equal to 
broadly rounded anterior head lobe; inferior antennal sinus 
shallow. Antenna 1 not longer than antenna 2, segment 2 
short, segment 3 very short, flagellum shorter than peduncle; 
Antenna 2, flagellum shorter than peduncle. 

Mouthparts highly modified. Lower lip, inner lobes tall, 
outer lobes large, oblique to nearly horizontal. Mandible, 
molar forming a smoothly rounded protuberance beneath 6- 
8 slender blades; left lacinia with 6-7 rounded teeth; palp 
slender; segment 1 short, segment 2 weakly setose; segment 
3 with few pectinate inner marginal setae. Maxilla 1, outer 
plate short, broad, apical spines slender, innermost strongest. 
Maxilla 2, outer plate with heavy spinelike apical setae. 
Maxilliped, plates weakly armed; inner plate lacking distal 
“button” spines, outer plate, inner margin concave, apex 
weakly spined; palp short, segment 2 shortest, segment 3 
longest, with medio-distal row of spines; dactyl slender. 

Coxal plates 1-4 very deep, broad, much deeper than 
body plates; coxa 1 distinctly smallest, but not expanded 
distally; hind cusps 2-5 per plate, small. Gnathopods small, 
short, subequal, subsimilar, non sexually dimorphic; bases 
slender, anterior margin setose (more strongly in Gnathopod 
1); merus rounded distally; carpus shallow- setose behind, 
length about equal to propod; palm very short, convex, with 
few short spines at postero-distal angle, long hind margin 
with groups of pectinate setae; dactyl short, smooth. 

Peraeopods 3-7 short, segmental margins short-spinose; 
dactyls very short, body heavy, inner margin nearly straight, 
micro-crenulated. Peraeopods 5-7 regularly homopodous, 
coxae very deep, hind lobes rounded below; bases broad, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


120 


KEY TO SPECIES OF DACTYLOPLEUSTES 


1. Eyes large, deep, reniform; mandibular palp, segment 2 distinctly longer than segment 1; coxa 1 dist- 
inctly shorter than coxa 2; telson elongate; uropods 1 & 2 not modified 2. 

— Eyes medium, ovate, few large facets; mandibular palp slender, segment 2 little longer than 1; coxa 1 

slightly shorter than coxa 2; uropods 1 & 2 (male), inner ramus short, broad, weakly armed 

D. (Apodactylopleustes) obsolescens (p. 123) 


2. Maxilla 1, outer plate with 9 apical spine teeth; peraeopod 5, basis with angular postero-distal lobe; 
mandibular palp, segment 3 broad, with 7 inner marginal pectinate setae; maxilliped palp, segment 2 
subequal to 1, dactyl thick, tip pectinate; gnathopod bases nearly bare of setae . D, echinoicus (p. 120) 
— Maxilla 1, outer plate with 15 slender apical spine-teeth; peraeopod 5, basis smoothly rounded behind; 
mandibular palp, segment 3 slender, with 5 inner marginal setae; maxilliped palp, segment 3 shorter 
than either 1 or 3, dactyl slender, acute, not conspicuously pectinate; gnathopods 1 & 2, basis strongly 
setose anteriorly D. (Neodactylopleustes) echinoides (p. 121) 


evenly rounded behind. 

Pleon side plates medium deep, broad, smooth below, 
hind comers acuminate. Pleopod peduncles short, raim with 
reduced numbers of segments, not sexually dimorphic. 
Uropods 1 & 2 short, stout; rami suramceolate, margins 
serially spinose , tips not spinose . Uropod 3 , peduncle short, 
stout, rami broad-lanceolate, inner ramus distinctly the larger. 

Coxal gills largest on peraeopods 4 & 5, smallest on 
peraeopod 6. 

Taxonomic commentary. The three component species 
of the genus are sufficiently distinct to justify separate 
generic status. Although Hirayama (1988) recognizes D. 
obscolescens as a distinct subgenus, Apodactylopleustes 
(see key above), further subdivision must await analysis of 
more extensive material in which new taxa are anticipated. 


Gnathopod 1 weakly subchelate; basis slender, bare; carpus 
and propod slender, subequal; hind margin of propod with 3 
groups of setae. Gnathopod 2 , segment 5 lacking hind lobe, 
segment 6, hind margin strongly setose, palm very short, 
oblique, dactyl short. 

Pereopods 3 & 4, segment 5 < 4, hind margins with short 
spines; dactyl short, body with 5-6 prominent posterior 
pectinations, unguis slender, curved. Peraopods 5-7, coxae 
relatively deep ; bases expanded to different degrees , 5 sharply 
angled behind, 7 very broad, rounded, smooth behind; segment 
5 shorter than 4; dactyls with small marginal pectinations. 

Pleon plates 1-3, hindcomer slightly acuminate. Uropod 
3 stout, rami broad; inner ramus almost equal to peduncle 
slightly longer than half outer ramus; outer margin of the 
outer ramus bare, inner margin with 4 spines. 

Telson short almost parallel-sided; apex rounded, 
unarmed. 


Dactylopleustes echinoicus (Tzvetkova) 

(Fig. 39) 

Parapleustes echinoicus Tzvetkova, 1975:122, fig, 1. 
Dactylopleustes echinoicus Karaman & Barnard, 1979: 
1 12. — Barnard & Karaman, 1991 : 647. . 

Diagnosis. Female (5.0 mm): Head, rostrum small, 
shorter than lateral lobes. Eyes moderate, reniform, black. 
Antennae short, 1<2; segments of the peduncle and flagellum 
shortened and broad. Flagellum of antenna 1 of 8 segments, 
of antenna 2 of 5 segments. 

Upper Up, lobes slightly asymmetrical. Mandible, spine 
row with 12 slender short blades; incisor 7-dentate; palp 
strong; segment 3 longest, with 7 inner marginal pectinate 
"D" spines. Maxilla 1, palp segment 2 with 5 apical spines, 
segment 1 lacking shoulder seta. Maxilla 2, plates subequal 
Maxilliped, inner plate with 3 apical button spines; outer 
plate short, with stout apical spine snd slender seta; palp 
segment 3 slender, dactyl short, broad, with apical inner 
marginal pectinations. 

Coxal plates 1 and 2 rectangular, lower margin convex, 
hind comer with 2 cusps. Coxal plate 4 deeper than broad. 


Distributional ecology. Known only from Bering Is- 
land (Commander Islands, off the east coast of Kamchatka), 
reef south of Nikol’skoye village. 

D. echinoicus is an obligate symbiont of the sea urchin 
Strongylocentrotus polyacanthus. The peraeopod dactyls 
are modified for holding the cmstacean onto the body of the 
sea urchin, as if “wedged in”, and to move around the 
movable spines on the surface of the test. 

Taxonomic commentskry, Dactylopleustes echinoicus 
is phyletically more primitive than the other two species of 
the genus subsequently described from Asiatic and North 
American coast (pp. below). The dactyls of this genus are 
adaptive to a lifestyle of clinging to the spines and surfaces 
of sea urchin tests. A less sophisticated form of grasping 
dactyl was noted in Commensipleustes commensalis (Shoe- 
maker) (p. 82). In that species, the dactyl and expanded 
spinose propod of peraeopods 3-7 form a subchelate claw- 
like mechanism that enables the amphipod to cling to the 
pleopods of the spiny lobster Panulirus interruptus. Such 
morphological specializations underscore the high degree of 
adaptive radiation within subfamily Parapleustinae that is 
associated with a commensal lifestyle. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


121 



/ MX 2 / ^__v^;D CTYLX) ' MXPD 

Fro. 39. Dactylopleustes echinoicus (Tzvetkova). Female (5.0 mm). Bering Sea. (after Tzvetkova. 1975) 

DactylopUmte.echino^es , new species 14 long slender distally curved apical spines; palp 

^ broad, With 6 Stout apical spines. Maxilla 2, plates short, 

dactylopleustes echinoicus Au%tm 1985- 592? Rpm»rH A *2 heavy apical spines. Maxilliped 

KaramaC 1991: 647X^1? 1985.592?-Ban,ard& mner plate short, apex sloping inward, with 3 minute button 

spines; outerplate slender, inner margin excavate, apex with 
Material 2 setae; palp segment 2 short, 3 with 

BRITISH COLUMBIA pectinations near base of thin pectinate dactyl. 

Northern Vancouver I • ELB Stn Nlfi Port 1 distinctly shorter than 2, hind comer with 4 

1 Qo< rtnon ^ Setae, palm very short, oblique, overhung by stout dactyl. 


1995-0080. 

Diagnosis. Femaleov (3. 3mm); Head, rostrum as long 
as lateral head lobe. Eye deep reniform, black. Antenna very 
short. Antenna 1 peduncle 3 not larger than basal flagellar 
segment, flagellum 5-segmented. Antenna 2, flagellum 5- 
segmented. 

Upper lip, median notch sharp, shallow, lobes nearly 


- ' ' 1 — > “ ■ -'“““a ovwui uaci^i. 

Onathopod 2, basis less strongly setae; carpus longer, 
propod subrectangular, palm distinct, strongly convex,’ 
nearly vertical, hind margin with 3 setal clusters. 

Peraeopods 3 & 4, margins of bases lined with short 
setae; dactyls short, stout, inner margins with 10+ minute 
pectinations. Peraeopods 5-7 closely homopodous, bases 
broadly rounded behind; segment 4 widening distally; 


equal. Lowerlip,innerlobedeep,n;rrow broadly rounded behind, segment 4 widening distally; 

nearly horizontal. Mandible molar large, broadly rounded; beL”d ‘^^'*®'’°'^''“®'>'P«‘=*“a'« Coxa6deep 

spinerow with? slender blades; incisor 8-dentate;leftlacinia Plenn h' zt a j 

8-9 dentate; palp segment 2 relatively long; segment 3 with l * ' ^’^"‘*‘=°™®>'P’'od“ced, acuminate. Uropod 

4 inner marginal pectinate "D” spines. Maxilla fouter plate mar.' * "I’ “ peduncle, 

P nes.MdXllia i, outerplate margins strongly spinose. Uropod 3, inner ramus heavy. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


122 



Taxonomic & distributional commentary. The host 

echinoid has not been determined precisely. However, the 
sea urchin Strongyocentrotus purpuratus occurred com- 
monly at the type locality . The echinoid fauna of the region 
is diverse (Ricketts & Calvin, 1968) and would indicate that 
several other host-specific species of Dactylopleustes may 
yet be discovered in the North American Pacific region. 


thick, margins with 4-5 spines; outer ramus with 3 spines on 
each margin. 

Telson relatively long, length 2X width, apex smoothly 
rounding. 

Etymology, Combining the suffix "oides" - like, or sim- 
ilar to, the type species D. echinoicus. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


123 




Dactylopleustes (Apodactylopleustes) obsolescens, Hira- 
yama, 1988: 44, figs. 269-271. — Ishimaru, 1994; 54. 

Diagnosis. Male? (2.0 mm): head, rostrum equal to 
lateral head lobes. Eye oval, large, orange. Antennae relat- 
ively long. Antenna 1, peduncular segment 3 larger than 
adjacent flagellar segment; flagellum 6-segmented. Antenna 
2, peduncular segments 4 & 5 slender, subequal ; flagellum 5- 
segmented. 

Lower lip, outer lobes nearly vertical. Mandible, molar 


process evanescent spine row with 5 short blades; incisor 7- 
8 dentate; left lacinia 8-9 dentate; palp segment 2 very short; 
segment 3 long and slender with 1 -2 inner marginal pectinate 
“D” spines. Maxilla 1, outer plate with 11 apical spines; 
palp, terminal segment apically truncate, with 5 spines! 
Maxilla 2, outer plate much the stouter, with 3-5 apical 
spines. Maxilliped, inner plate apically truncate, lacking 
button spines; outer plate slender, inner margin excavate; 
palp segment 2 short, distally pectinate, dactyl pectinate. * 
Coxa 1 not noticeably shorter than 2, hind comer with 2 
cusps. Coxae 2-3 with 2-3 hind cusps. Coxa 4 relatively 
broad, hind process curved upwards. Gnathopod 1, basis 
weakly setose; carpus stronger than propod, dactyl stout. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


124 


overhanging short, vertical palm. Gnathopod 2, basis nearly 
bare; propod rectangular, slightly longer than carpus, dactyl 
overhanging short vertical palm, hind margin with 2 groups 
of setae. 

Peraeopods 3 & 4, hind margins of segment 4-6 with 
regular spines, dactyl finely pectinate behind. Peraeopods 5- 
7 irregularly homopodous, bases unevenly expanded, hind 
margins nearly straight, 6 relatively narrow, 7 broadest, hind 
lobes deep; segment 4 broad; segment 5 short, 6 relatively 
long; dactyls thick, anterior margins very finely pectinate. 

Pleon plate 3 hind comer strongly produced acuminate. 
Uropods relatively stout, rami short, broad, especially outer 
ramus, much shorter than peduncle, margins weakly spinose. 
Uropod 3, inner ramus, margins each with 3 spines; outer 
ramus, our margin with 2 pines, inner margin bar. Telson 
medium short, length 1.7 X width, apex evenly rounded. 

Distribution. Ariake Sea (1 specimen only). 

Taxonomic commentary. Dactylopleustes obsolescens 
is clearly distinct from echinoicus, but more closely similar 
to echinoides. It is distinctive in the unlike form of peraeopods 
5-7, the short, weakly armed uropods, and the very elongate 
mandibular palp segment 3. 

Pleusirinae Bousfield & Hendrycks, 1994 

Pleustidae Gurjanova 1972: 135, 138 (key) (part).— Barn- 
ard & Karaman, 1991; 649. 

Pleusirinae Bousfield & Hendrycks, 1994; 40. 

Type genus. Pleusirus Barnard, 1969b, original des- 
cription. 

Diagnosis. Body small, slender, dorsally smooth; 
urosome 2 occluded dorsally. Head, rostrum short, deflexed, 
anterior head lobe broadly rounded. Eye rounded. Antennae 
slender, medium, antenna 1 the longer. Antenna 1 , peduncles 
2 & 3 short; accessory flagellum minute, apex setose; an- 
tenna 2, peduncle medium strong. 

Mouthparts strongly modified. Upper lip broad, lobes 
asymmetrical. Lower lip, inner lobes deep, narrow. Mandi- 
ble, molar reduced to a large smooth lobe; spine row short, 
blades short; left lacinia multi-dentate (9-10); right lacinia 
lacking; palp slender, segment 2 longest; segment 3 shorter, 
lacking baso-facial seta; segment 1 elongate. Maxilla 1, 
inner plate small, bare; outer plate with 9 apical spines; palp 
slender, facially pilose, apex weakly armed. Maxilla 2, 
plates small, weakly setose-spinose. Maxilliped, inner plate 
short, with few apical and inner marginal spines; outer plate 
narrow, colunmar; palp large, subcheliform; segment 3 wid- 
est medially, not produced beyond base of slender dactyl. 

Coxal plates 1-4 increasing in size posteriorly, rounded 
below, lacking hind cusps. Gnathopods 1 & 2 slender, 
subequal, “eusiroidean” in form, not sexually dimorphic; 


carpus elongate, hind lobe shallow; propod subovate, palm 

long, lacking median tooth; posterior angle with 2 spine 

clusters. 

Peraeopods 3-7 slender; dactyls short. Peraeopods 5-7 
closely homopodous in size and form; bases broad, rounded 
behind; segment 4 little overhanging segment 5 behind. 

Pleon plates 1-3, hind comers acuminate. Pleopods 
strong, not sexually dimorphic. Uropods 1-3 slender, rami 
elongate, spinose. Telson elongate, keeled proximally,pem- 
icillate setae median. 

Coxal gills narrow, saclike on peraeopods 2 & 3, plate- 
like on peraeopods 4-6, increasing posteriorly. 

Taxonomic commentary. The subfamily appears 
allied with the subfamily Parapleustinae in most character 
states, especially of the mouthparts. It is unique in the 
eusiroidean form of the gnathopods, the generally reduced 
form of maxillae 1 & 2, the inflated, distally smooth 
mandibular molar; elongate mandibular palp segment 1 ; and 
the semi-subchelate form of the maxilliped palp. 

Pleusirus J. L. Barnard 

Pleusirus J. L. Barnard, 1969b: 204.— Gurjanova, 1972: 
135. — Barnard & Karaman, 1991: 649. 

Type species. Pleusirus secorrus Barnard, 1969b: 204. 

Subspecies. Pleusirus secorrus asiaticus Kudrjaschov 
& Tzvetkova, 1975, original designation. 

Diagnosis. With the characters of the subfamily , and in 
addition: Antenna 1, peduncular segment 1 with postero- 
distal process; flagellar segments, posterior marginal aesth- 
etascs paired, prominent. 

Mandibular blades thick, distally pectinate; incisor 7-8- 
dentate, third tooth largest. Maxilla 1, palp segment 1 with 
"shoulder" seta. Maxilla 2, inner plate not broadened, lack- 
ing inner marginal plumose seta. Maxilliped, inner plate 
with stout inner marginal and apical spines. 

Gnathopods 1 & 2, bases slender, margins not strongly 
setose; propod, hind margin smooth; dactyl slender. 

Peraeopods 5-7, coxae deep, postero-lobate, hind lobes 
rounded, segment 5 not longer than 4. 

Uropods 1 & 2, inner ramus longer than peduncle. Uro- 
pods 2 & 3, outer ramus short. Telson rounded, penicillate 
setae median. 

Male; Antennal segments with prominent aesthetascs; per- 
aeopods 5-7 relatively slender; dactyls relatively long, slender, 
nearly straight. 

Taxonomic and distributional commentary. The genus 
encompasses two forms, one a subspecies of the other, one 
on the Asiatic and the other on the North American Pacific 
coast. 


AMPHIPACIFICA VOLII no. 1. AUG. 31, 1995 125 



Pleusirus secorrus J. L. Barnard, 1969b: 204, fig. 56.— 

Guijanova, 1972: 135, 138 (key). — ^Austin, 1985: 592. 

Staude, 1987: 379. — Barnard & Karaman, 1991; 650. 

Material examined. 

ALASKA. 46 specimens (all females, afew subadults) from 
18 localities, as follows: 

Southeastern Alaska: ELB Stns., June-July, 1961: A3 (8); 

A6 (12); A8 (1); A48 (1); A75 (3); A80(7); A8 1 (1); A92 (6); 


BRITISH COLUMBIA. 252 specimens (including 1 male?) 
at 59 localities, as follows; 

Queen Charlotte Islands. ELB Stns., July- Aug 1957- H14 
(2);W4a(2);W4b(3); E5(1);E25(1);W8(7); W9(1V W 1 1 
(7);W12a(3). 

Northcentral coast. ELB Stns., July, 1964: HI (15)- H3 (2)- 
H5 (30); H7 (12); H8 (2); HIO (2); H12 (8); H26 (5)- H 23 
(1)H29 ( 1); H30 (10); H47 (1); H48 (2); H50 (3); H53 (20+)- 
H57 (1); H65 (6). ELB Stn., 1959: N22 (2). 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


126 


Vancouver Island, north end: ELB Stns., July, 1959: 01 (1); 

05 (3); 01 1 (3); 013 (7); 015 (7); V5 (2); V7 (3); VI 1 (1); 

V17 (2); V18 (1); N 1 1 (1); N16 (1). 

Vancouver Island, south end: ELB Stns., July-Aug., 1955: 
FI (6); F4 (1); P2 (1); P7 (1). ELB Stns., 1970: P715 (1); 
P716(2); P718(13);P719(1). ELB Stns., 1975:P5b(2);P5c 
(1); (20(4). ELB Stns., 1976:B3(2);B4(2);B5(1); B7(10). 
ELB Stns., 1977: B7a ( (8); Bllb (1); B14 (1); B19b (2); 
B21b (3). ELB Stn. 015, Box I., Wickaninnish Bay, in 
Phyllospadix clumps, algal mats, over bedrock, LW level, 
Aug. 16, 1959 - female ov (3.7 mm) (slide mount) (fig’d 
specimen) + 7 other females. 

Duncan Bay, Middle Pt., barge, 3-4 m dive, tZ/va &bryozo- 
ans,P.Shawcoll.,Seot5, 1987- 1 male (fig’d) + 6 specimens. 

WASHINGTON-OREGON. 22 specimens at 3 localities, as 
follows: 

Coastal localities: ELB Stns, July-Aug., 1966: W40 (18); 
W42 (2); W58 (2). 

Diagnosis. With the characters of the genus and sub- 
family. The subspecies Khudrjaschov& Tzvetkova, 

1975, may prove to be morphologically, if not ecologically, 
distinct, but western Pacific material was not re-examined in 
this study. 

Distributional ecology. On the North American Pacific 
coast this species occurs from southeastern Alaska, through 
British Columbia, Washington and Oregon, to southern Cal- 
ifornia. It occurs commonly from the extreme LW level to 
to depths of 25 m, in clumps of Phyllospadix, algae, and in 
organic debris, often on shelly sand bottoms, mainly at cold, 
high salinity, outer coast locations. 

Pleusirus secorrus asiaticus Kudrjashov & Tzvetkova 

PleusirussecorrusasiaticusK.udTi3shov&TzyQlko\3i, 1975: 
1314, fig. 2A. — Tzvetkova Kudryashov, 1985: 1. 

Pleusirus secorrus Ishimaru, 1985d: 103. — Ishimaru, 1994: 
54. 

Taxonomic and distributional commentary. This form 
was collected from clumps of algae and Phyllospadix at 
stations on South Sakhalin I., in the southern part of the Sea 
of Okhotsk, and south to Pos'yet Bay in the Sea of Japan. It 
is also recorded from amongst fronds of Tichocarpus carin- 
atus, Cytoseira sp., and Laminaria japonica. Females with 
eggs and early juveniles occur in July and August. 

The Asiatic form of P. secorrus has been synonymized 
by Ishimaru (loc. cit.) and Barnard & Karaman (loc. cit.). 
However, taxonomic differences noted in the original 
description (Kudrjashov & Tzvetkova, loc. cit.) suggest that 
a different species may be involved. In order to justify 
recognition of asiaticus as a full species, it is recommended 
that the original material be re-examined, redescribed and 
fully figured. 


Systematic and Biogeographical Analyses 

This study treats the systematics and distributional 
ecology of 29 species of the gammaridean subfamily 
Parapleustinae that occur along both Asiatic and North 
American coasts of the North Pacific region. A modified 
phenetic cluster analysis, and corresponding cladistic analysis, 
indicated the Parapleustinae to be the most advanced 
phyletically of the 12 recognized subfamilies within family 
Pleustidae (Bousfield & Hendrycks, 1994). We conclude 
here by commenting in greater detail on aspects of the 
morphology and lifestyle and on biogeographical rel- 
ationships of its component genera and species. 

The seven genera of Parapleustinae appear similar in the 
overall plesiomorphic form of the body and appendages. 
Greatest morphological diversity occurs in the numbers and 
kinds of mandibular blades, in the cutting edges of the 
incisors and left lacinia, and to lesser extent in the form and 
armature of the gnathopods. Sexually dimorphic gnathopods 
occur, uniquely in this subfamily, among the Pleustidae.The 
taxonomic and phyletic relationships of the seven genera are 
not readily apparent through general inspection, but may be 
clarified through numerical analysis of characters and 
character states of those body features (Fig. 43,' page 127). 
For this purpose, a modification of the UPGMA cluster ana- 
lysis system of Sneath and Sokal (1973) is utilized. The 20 
selected taxonomic characters and corresponding character 
states are outlined in Table I. The overall degree of 
evolutionary advancement of the genus is provided by a 
plesio-apomorphic (P.-A.) index, derived by summing the 
values for each character state for each species, as explained 
in previous analyses (e.g. Bousfield and Hendrycks, 1994; 
Jarrett & Bousfield, 1994). 

The phenogram of morphological relationships (Fig. 
43) suggests that the seven genera are not very closely 
similar, at least in the characters considered. Only two 
generic pairs, the North American endemic Gnathopleustes- 
Trachypleustes, and the broadly temperate-subtropical 
Incisocalliope-Commensipleustes cluster at similarities of 
70% or better. The pan-Pacific genera Micropleustes and 
Parapleustes cluster at 60-65% with the latter complex. 
However, the mainly North American genus Chromopleustes 
stands in isolation, with less than 50% similarity to the other 
generic groupings. The P.-A. index is slightly less than 20 
(less than 50% of maximum apomorphy) for all genera 
except the relatively advanced genus Incisocalliope where 
the value is 30 (75% of maximum). These values may 
indicate that the members of the Parapleustinae are 
evolutionary “stable”, i. e., they remain “locked in” to 
exploitation of specialized shoal-water niches (e.g., within 
Phyllospadix communities) of the North Pacific region that 
either do not exist elsewhere (e.g., in the cold-temperate 
North Atlantic or antiboreal regions), or else are inaccessible 
because of past and present physical and physiological 
barriers to dispersal. 

A phenogram of morphological relationships within 
species of the genus Incisocalliope is provided in Figure 44, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


127 


B 


t 

40 

1 

38 

>- 


H 

36 

CC 


< 

34 



i 

32 

(/) 


Id 

30 

1- 


< 

28 



(/) 

26 

n 

Id 


1- 

24 

O 


< 

cc 

22 

< 


X 

20 

o 


Q 

18 

Ld 


cc. 

16 

< 


a. 

1 

14 

1 

12 


18 


17 


19 


17 


10 


19 


30 P.-A. INDEX 


GENERA 

A - Ch ro m o p / eu s t es 
B -Gnathop/eustes 
C - Trachyp/eustes 
D - Mi cro p / eu s tes 
E - Parap/eu stes 
F - Co m m en sip / eu s tes 
G - in ci s o cai i i o p e 


75 “ 

f£ 


50 


0) 


FIG. 43. PHENOGRAM OF GENERA OF SUBFAMILY PARAPLEUSTINAE 


p. 129. The analysis is based on 16 characters and cor- 
responding character states orvided in Table II, p. 1 30. The 
8 species cluster into three main assemblages at similarities 
of 65-75%, viz., a relatively primitive newportensis-bairdi 
group, a very advanced dilatatus-makiki group, and a 
slightly less advanced derzhavini-aestuarius group of two 
closely similar species pairs. These three major assemblages 
cluster at about the 50% similarity level and appear therefore 
not closely related. The newportensis-bairdi subgroup, 
known only from inshore waters of southern California, is 
especially plesiomorphic in character states of themouthparts 
and peraeopods, but the gnathopods are powerfully 
subchelate, and relatively advanced. 

Possible biogeographical relationships of the dilatatus- 
makiki group are discussed below (pp. 129-30). The close 
similarity of the regionally co-occurring sibling species pair 
of derzhavini and is not unexpected. However, 

the 90% morphological similarity between the widely 
separated Asiatic Pacific and the North American 

Atlantic aestuarius is unexpected and defies ready explan- 

ation. 


Similar analysis of the North American endemic genus 

Gnathopleustes suggests th^t G. pugettensis,a simplex, G. 
pachychaetus and G. den form a relatively advanced and 
closely related species complex that collectively have a 
continuous distribution from southeastern Alaska to southern 
California (Table II, p. 129). Gnathopleustes trichodus ond 
G. JerratMj are relatively primitive morphologically, isolated 
phyletically and more restricted distributionally. The 
Trachypleustes species complex, with highly modified 
mandibular blades, and possibly more speciose than here 
considered, is more northerly in distribution. At least one 
species attains the Bering Sea region but has not yet been 
taken on the Asiatic coast. The Micropleustes complex is 
more speciose on the Asiatic coast. However, the most 
common North American species of this genus, M nautilus, 
has die widest range of any parapleustin in the North American 
Pacific region, from the Bering Sea to southern California. 
With respect to subfamily Pleusirinae, Pleusirus secorrus, 
including its Asiatic subspecies, is the only known member 
of family Pleustidae to occur in all nine biogeographic zones 
of the North Pacific region. Subfamily Dactylopleustinae is 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


128 


TABLE I. CHARACTERS AND CHARACTER STATES: GENERA OF PARAPLEUSTINAE 



CHARACTER STATES 

CHARACTERS 

Plesiomorphic 

0 

Intermediate 

1 

Apomorphic 

2 

1. Antennal, peduncular 

long 


short 

segment 2: segment 1 



short 

2. Antenna 2, peduncular 

long 


segments 4 & 5 

3. Upper lip, lobes 

shallow 

subequal 


deep, markedly 
asymmetrical 

4. Lower lip, inner lobes 

deep 

narrow 


shallow 

broad 

5. Mandibular blades 

numerous (>10) 

(7-8) 

few (~5) 


long, slender 

short, acute 

short, flat 

6. Mandible, palp segment 3, 

12-15 

8-10 

-5 

number of “D” spines 



10 + 

7. Mandibular left lacinia, 

5-6 

7-9 

number of teeth 


11 

15+ 

8. Maxilla 1, outer plate. 

9 

number of apical spines 


1 


9. Maxilla 1, palp segment 1, 

0 

2 

number of setae 




10. Maxilla 2, width of 

narrow 


broad, 

inner plate 

L>W 


L-W 

11. Maxilliped, inner plate, 

7-10 


0-2 

number facial setae 



large 

12. Maxilliped, segment 3 

short 


13. Gnathopods 1 & 2, 

weak 


strong 

size of propod 

shallow 


deep 

14. Gnathopods 1 & 2, 

elongate 


short 

size of carpus 

shallow 


deep 

15. Gnathopods 1 & 2, degree 

none 


marked 

of sexual dimorphism 




16. Gnathopods 1 & 2, 

strong 

vestigial 

lacking 

palmar tooth 



3-4 

17. Coxae 1-3, number of 
posterior marginal spines 

none 


18. Peraeopods 3-7, size of 

subequal 


5 distinctly 
shorter 

segment 5: segment 4 



19. Uropods 1 & 2, 
ramal spines 

numerous 

strong 


few 

weak 

20. Telson shape 

short 

broad 


elongate 

narrow 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


129 


I 

> 

H 

(L 


32 
30 
28 
< 26 



(/) 

LU 

I- 

< 

I- 

(0 

CE 

LU 

I- 

o 

< 

a: 

< 

X 

o 

o 

lU 

cc 

< 

Q. 


24 

22 

20 

18 

16 

14 

12 

10 


INCiSOCALLtOPE 


A - 

n e wp orten si 8 

B - 

bairdi 

C - 

diiatatu s 

D - 

makiki 

E - 

nipponensis 

F - 

derzh a vini 

G - 

aestuarius 

H - 

fi tiai is 


75 


QC 

< 


50 


(/) 


FIG. 44. PHENOGRAM OF SPECIES OF INCISOCALUOPE 


represented on Asiatic and North American coasts by the 

species pair of Dactylopleustes obsolescens and D. echin- 
oides, respectively. Although these echinoid-commensal 
species probably have geographical ranges similar to their 
host species of Strongylocentrotus, locality records are yet 
insufficient for meaningful biogeographical analysis. 

Biogeographical considerations 

The subfamily Parapleustinae is essentially endemic to 
continental coasts of the North Pacific region (Table III, p. 
131). The distribution of five of the seven genera (i.e. 
Chromopleustes, Micropleustes, Gnathopleustes, 
Trachypleustes and Commensipleustes) is essentaially cold- 
temperate, whereas Parapleustes is subarctic-boreal, and 
Incisocalliope is temperate-subtropical. Of its 28 described 
species here included, only three species have been recorded 
elsewhere, Viz., Parapleustes gracilis from arctic-subarctic, 
marine parts of the N orth Atlantic and western Arctic Oceans ; 
Incisocalliope aestuarius from temperate estuaries of the 
western North Atlantic, and 1. makiki from the Hawaiian 
Islands in the south-central subtropical North Pacific. 

In the northern North Pacific region, 16 species of 


parapleustins, representative of all seven genera, occur along 
the coasts of continental North America, whereas only nine 
species, in four genera, have been recorded to date from the 
Asiatic continental coast (Table III). In the eastern North 
Pacific, species numbers are largest along the coast of British 
Columbia ( 1 0 species in each of zones 5, 6) but decrease both 
northwards and southwards. In the western North Pacific, 
the fauna of the Asiatic coast is less well known, but most (7) 
parapleustin species occur in the northern part of the sea of 
Japan, and fewer (3) in the cold waters of the Sea of Okhotsk 
to the north. Although no single species has yet been 
recorded from both continental coasts, the Bering Sea contains 
five species in four genera, and presumably provides the 
major pathway of gene flow between the two continental 
populations. 

However, North American species of Incisocalliope 
(i.e. newportensis and bairdi) are widely separated from 
their Asiatic counterparts (e.g.filialis, derzhavini, nipponensis 
and dilatatus) and are relatively primitive morphologically 
(Fig. 44, above). These facts would suggest that these 
populations have been separated geographically for a 
considerable time, perhaps since the early Palaeogene (50- 
60 m.y.b.p.) when northern Pacific sea levels were lower, 
and marine climates were warmer and more equable (Adams, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


130 


TABLE n. CHARACTERS AND CHARACTER STATES: INCISOCALUOPE SPECIES 


CHARACTER 

CHARACTER STATE 


Plesiomorphic 

Intermediate 

Apomorphic 


0 

1 

2 

1. Antenna 1, number 

30+ 

~25 

<15 

flagellar segments 




2. Antenna 2, number 

20+ 

10-15 

-5 

flagellar segments 




3. Mandible, palp seg. 3, 

~10 


-5 

number “D” setae 




4. Mandible, number 

10 


5 

of blades in row 




5. Maxilla 1, palp 2, 

4 


0 

number facial setae 




6. Maxilliped, inner pi.. 

4+ 

3 

2 

apical “button” spines 




7. Gnathopodl, basis. 

nearly bare 


strong 

ant. marginal setation 



throughout 

8. Gnathopod 1, carpal 

broad 


narrow 

lobe 

shallow 


deep 

9. Gnathopod 1, posterior 

3 


0 

margin, no. setal gps. 




10. Peraeopods 3 & 4, 

subequal 


markedly 

segments: segment 4 



shorter 

11. Peraeopods 5-7, 

broad 


narrow 

width of basis 

width-depth 


width« depth 

12. Peraeopods 5-7 

deep, reaching 


shallow 

hind lobe depth 

segment 4 



13. Uropod 1, peduncle 

numerous 


few (4) 

outer marginal spines 

(10+) 


basal position 

14. Uropod 2, length 

long 


markedly 

of outer ramus: inner 

subequal 


shorter 

15. Uropod 3, length 

long 


short 

outer ramus: inner 

(75%+) 


(-60%) 

16. Telson, rel. form 

long, slender 


short, broad 


1981). During that period, and perhaps later, early members 
of the genus may have penetrated via a southern waterway 
(now blocked by the Panamanian isthmus) to the western 
Atlantic region where Incisocalliope aestuarius remains a 
sole survivor. The widely disjunct distributions of the 
filialis-aestuarius species pair is also reminiscent of somewhat 
similar disjunct distributions of the coastal aquatic arachnid 
order Xiphosurida (Savory, 1964), and the coastal aquatic 
reptilian genus Alligator (Carr, 1963). Both these groups 
may have been biogeographically continuous between 
southern Asia and North America during early to middle 
Cretaceous times, via a Tethyan marine pathway outlined by 
Howarth (1991). Such a hypothesis is unlikely for para- 
pieustins and related subfamily members of which no relict 
modern representatives now exist along that route and/or are 
physiologically unsuited to those marine thermal regimes. 
The presence in the remote Hawiaiian islands of Incisocalliope 
makiki, closely related to /. dilatatus of the Asiatic group. 


is anomalous. However, /. makiki may prove to be a relict 
species, representative of an ancestral group from Japan that 
penetrated the Hawaiian Archipelago, perhaps during the 
early Tertiary. They may have survived by “island hopping” 
as the volcanic islands of the chain successively emerged in 
the east and eroded away in the west (Howarth & Mull, 
1992). 

In summary, subfamily Parapleustinae encompasses 
diverse, relatively advanced morphotypes and specialized 
lifestyles of pleustid micropredators. These occupy various 
niches within the Phyllospadix and sessile invertebrate 
communities of intertidal and shallow water habitats, almost 
exclusively within the North Pacific region. Although this 
fauna is believed relatively ancient, and probably originated 
during Mesozoic times (Bousfield, 1982b), the long-term 
stability of regional shallow-water ecosystems and their 
marine climates may have been major factors in dampening 
evolutionary thrust in other directions. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


131 


TABLE III . DISTRIBUTION OF GENERA AND SPECIES OF PARAPLEUSTINAE 

IN THE NORTH PACIFIC REGION. 


TAXON 


BIOGEOGRAPHIC 

ZONE 



1 

2 

3 

4 

5 

6 

7 

8 

9 

1 . Chromopleustes 










C.johanseni 


X 

JC 







C. oculatus 



X 

X 

X 

JC 




C. lineatus 




X 

X 

X 

JC 



2. Micropleustes 










longimanus 

X 

X 








behningioides 

X 









behningi 

nautilus 

X 


X 

X 

X 

X 

X 

X 

X 

nautiloides 






X 

X 

X? 


3. Parapleustes 










ishimarui 
americanus 
gracilis * 


JC 

X 

X 

X 

X 




4. Gnathopleustes 










serratus 




X 

X 

X 

X 

X 


pachychaetus 




X 

X 

X 

X 



trichodus 





X 





simplex 





X 





pugettensis 




X 

X 

X 

X 

X 

7 

den 








X 

X 

5. Trachypleustes 










trevori (+ varieties) 



X 

X 

X 

X 

9 



vancouverensis 






X 




6. Commensipleustes 










commensalis 








7 

X 

7. Incisocalliope 










filialis 

X 









derzhavini 

X 









nipponensis 

X 









dilatatis 

makikU 

newportensis 

X 








X 

bairdi 

aestuarius+ 









X 


* N. Atlantic-subarctic; ! Hawaiian Islands; + N. American Atlantic temperate 
BIOGEOGRAPHIC ZONES; 

1. Sea of Japan; 2. Sea of Okhotsk; 3. Bering sea and Aleutians; 4. Southeastern Alaska; 5. Northern 
B. C.; 6. Southern B. C.; 7. Wash.-Oregon; 8. Northern California; 9. Southern & Baja California. 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


132 


REFERENCES 

Adams, C.G., 1981. An outline of Tertiary palaeogeography. 
Chapter 14; 221-235. ijL P.H. Greenwood (ed.). The Ev- 
olving Earth. British Museum. Cambridge Univ. Press. 

Anderson, R., 1988. Occurrence of toxic biochemical com- 
pounds in marine invertebrate animals. Trans. Roy. Soc. 
Canada, 5 (6): 

Austin, W. C., 1985. Annotated checklist of marine invert- 
ebrates in the cold temperate northeast Pacific. Khoyo- 
tan Marine Laboratory, Vols. I-III; 1-682. 

Barnard, J. L., 1952. Some Amphipoda from central Cali- 
fornia. Wasmann Jour. Biol. 10: 9-36, 9 pis. 

, 1954. Marine Amphipoda of Oregon. Oregon 

State Monographs. Studies in Zoology 8: 1-103, 33 pis. 

, 1956. Two rare amphipods from California 

with notes on the genus Bull. S. Calif. Acad. Sci., 

55: 35-43, pis. 12-14. 

, 1959. Estuarine Amphipoda ini Ecology of 

Amphipoda and Polychaeta of Newport Bay, California. 
Occ. Pap. Allan Hancock Foundation 21: 13-69, 14 pis. 

, 1969a. The families and genera of marine 

gammaridean Amphipoda. U. S. Natl. Mus. Bull. 271: 
1-535. 

, 1969b. Gammaridean Amphipoda of the rocky 

intertidal of California: Monterey Bay to La Jolla. Natl. 
Mus. Bull. 258: 1-230, figs. 1-173. 

, 1970. Sublittoral Gammaridea (Amphipoda) 

of the Hawaiian Islands. Smiths. Contr. Zool. 34:1-286 

, & R. R. Given, 1960. Common pleustid am- 
phipods of southern California, with a projected revis- 
ion of the family. Pacific Naturalist 1(17): 37-48. 

, & G. S. Karaman, 1980. Classification of 

gammarid- Amphipoda. Crustaceana, Suppl. 6: 5-16. 

, 1982. Classificatory re- 
visions in gammaridean Amphipoda (Crustacea) Part 2. 
Proc. Biol. Soc. Wash. 95(1): 167-187. 

, 1991. The Families and 

Genera of Marine Gammaridean Amphipoda (Except 
Marine Gammaroids). Parts 1 & 2. Records Australian 
Museum, Suppl. 13: 1-866, iilustr. 

Boeck, A., 1871. Crustacea Amphipoda borealia et arctica. 
Forh. Vidensk.-Selsk. Krist. 1870: 83-279. 

, 1 872. Bidrag til Califomiens Amphipoden fauna 

Forh. Vidensk.-Selsk. Krist. 1871, 22 pp., I pi. 

Bousfield, E. L., 1958. Ecological investigations on shore 
invertebrates of the Pacific coast of Canada, 1955. Bull. 
Natl. Mus. Canada, 147: 104-115. 

, 1963. Investigations on sea-shore inverte- 
brates of the Pacific coast of Canada, 1957 and 1959. 1. 
Station list. Bull. Natl. Mus. Canada 185: 72-89. 

, 1968. Studies on littoral marine inverte- 
brates of the Pacific coast of Canada, 1964, 1: Station 
list. Bull. Natl. Mus. Canada 223: 49-57. 

, 1982a. Amphipoda. Gammaridea. In: S. P. 

Parker [ed.]. Synopsis and Classification of Living 


Organisms, McGraw Hill, New York, N.Y. vol. 2; 254- 
285, and 293-294. 

— ,1982b. Amphipoda. Palaeohistory. In Mc- 
Graw-Hill Yearbook of Science and Technology for 
1982-1983. S. P. Parker [ed.]: 96-100. 

, 1985. Mysterious insects of the sea. Rotunda 

(ROM, Toronto) 18 (3): 30-36. 

, & E. A. Hendrycks, 1994. A Revision of the 

Family Pleustidae (Crustacea: Amphipoda: Leucothoi- 
dea). Part 1. Systematics and biogeography of compon- 
ent subfamilies. Amphipacifica I (1); 17-57. 

, & N. E. Jarrett, 1981. Station lists of marine 

biological expeditions of the National Museum of Nat- 
ural Sciences in the North American Pacific coastal reg- 
ion, 1966 to 1980. Syllogeus 34, 66 pp. 

, & D. E. McAllister, 1963. Station list of the 

National Museum Marine Biological Expedition to 
southeastern Alaska and Prince William Sound. Bull.Natl. 
Mus. Can. 183: 7 6-103. 

, & C.-t Shih, 1994. The Phyletic Classification 

of Amphipod Crustaceans: Problems in Resolution. 
Amphipacifica 1(3); 76-134. 

Buchholz, R, 1874. Crustacean: Die zweite deutsche Nord 
polarfahrtinden Jahren, 1869 und 1870 unter Fuhrung 
des Kapitan Karl Koldewey. vol. 2, Wissenschaft. Er- 
gebn. 11, Zool: 262-399. 15 pi. 

Bulycheva, A. N., 1952. New species of amphipods (Am- 
phipoda: Gammaridea) from the Sea of Japan (in Russ- 
ian). Trud. Zool. Inst. Akad. Nauk, SSSR. 12:195-251. 

Carr, A., 1963. The Reptiles. Time Inc., New York, N. Y., 
192 pp. 

Cole, G. A., 1980. The mandibular palps of North Ameri- 
can fresh water species of Gammarus. Crustaceana, 
Suppl. 6: 68-83. 

Dana, J. D., 1853. Crustacea. Part II. United. States Expl- 
oring Expedition 14: 689-1618, 96 pis. 

Dunbar, M. J., 1954. The Amphipoda Crustacea of Ung- 
ava Bay, Canadian Eastern Arctic. Jour. Fish. Res. Bd. 
Canada 11; 709-798. 42 figs. 

Fox, R. S., & K. H. Bynum, 1975. The amphipod crusta- 
ceans of North Carolina estuarine waters. Chesapeake 
Science 16: 223-237, 3 figs. 

Gurjanova, E. F., 1938. Amphipoda Gammaroidea of Sia- 
ukhu Bay and Sudzukhe Bay (Japan Sea). Reports of 
the Japanese Hydrobiological Expedition of the Zool- 
ogical Institute of the Academy of Sciences, USSR, 
in 1934. 1: 241-404, 59 figs. (In Russian). 

, 1951. Bokoplavyi Morei SSSR, i sop- 

redelnyk vod. Opred. Faune SSSR, Izdel. Zool. Inst. 
Akad. Nauk. No. 41. 1029 pp. 

, 1972. New species of amphipods (Amphi- 
poda, Gammaridea) from the northern part of the Pac- 
Pacific Ocean. Trud. Zool. Inst. Akad. Nauk SSSR, 
52: 129-200, figs: 1-42 (in Russian). 

Hirayama, A., 1988. Taxonomic studies on the shallow- 
water Gammaridean Amphipoda of West Kyushu, 
Japan VIII. Pleustidae, Podoceridae, Priscomilitaridae, 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


133 


Stenothoidae, Synopiidae, and Urothoidae. Publ. Seto 
Mar. Biol. Lab. 33(1/3): 39-77, figs. 265-271. 

Holmes, S. J., 1908. The Amphipoda collected by the U.S. 
Bureau of Fisheries Steamer “A /tore off the west 
coast of North America in 1903 and 1904 with descrip- 
tion of a new family and several new genera and spec- 
ies. Proc. U. S. Natl. Mus. 35 ( 1654): 489-543. 

Howarth, F. G., & W. P. Mull, 1992. Hawaiian Insects and 
their kin. Univ. Hawaii Press, Honolulu. 160 pp., 152 pis. 

Howarth, M. K., 1981. Palaeogeography of the Mesozoic. 
Ch. 13: 197-220. in The Evolving Earth. P. H. Green- 
wood (ed.). British Museum, Cambridge Univ. Press. 

Irie, H., & K. Nagata, 1962. A list of the benthic Crusta- 
cea known in Ariake Sea. Bull. Fac. Fish., Nagasaki 
Univ., 13: 19-24. 

Ishimaru, S., 1984. Taxonomic studies of the family Ple- 
ustidae (Crustacea, Amphipoda, Gammaridea) from 
coastal waters of Northern Japan. 1. The genus P«ra- 
pleustes. Fac. Sci. Hokkaido Univ., ser. vi., Zool. 23 
(4): 403-453. 

, 1985. Taxonomic studies of the family Ple- 

ustidae (Crustacea, Amphipoda, Gammaridea) from 
coastal waters of Northern Japan. II. The Genus P/^m- 
symtes. Fac. Sci. Hokkaido Univ., ser. vi, Zool. 24 
(1): 43-69. 

, 1994. A catalogue of gammaridean and in- 

golfiellidean Amphipoda recorded from the vicinity of 
Japan. Report Sado Marine Biol. Station, Niigata Uni- 
versity No 24: 29-86. 

Jarrett, N. E., & E. L. Bousfield, 1994. The amphipod sup- 
erfamily Phoxocephaloidea on the Pacific coast of N. 
America. Family Phoxocephalidae. Part 1. Metharpini- 
inae, new subfamily. Amphipacifica 1(1): 58-140. 

Karaman, G. S., & J. L. Barnard, 1979. Classification re- 
visions in gammaridean Amphipoda (Crustacea) Part 1 
Proc. Biol. Soc. Wash. 92 (1): 106-165. 

Kroyer, H., 1838. Gronlands amfipoder beskrevne af Hen- 
rik Kroyer. Danske Vidensk. Selsk. Naturvid. Math. 
Afhandl. 7: 229-326, 4 pis. 

Kudrjaschov, V. A., 1972. K faune i ekologii bokoplavov 
(Amphipoda- Gammaridea) privilo-otlivnoi zony Kuril' 
skikh ostrovov (Litoral’o-vov Iturup, Urup, Simuschir, 
Paramuschir). Uchenye Zapiski Dvgu 60: 79-116. 

, & N. A. Tzvetkova, 1975. New and 

rare species of Amphipoda Gammaridea from coastal 
waters of the South Sakhalin. Zool. Zhum. 54: 1306- 
1313, 3 figs. 

Lincoln, R. J., 1979. British marine Amphipoda: Gammar- 
idea. Brit. Mus. (Nat. Hist.), London. 1-658, 280 figs. 

Nagata, K., 1965. Studies on marine gammaridean Amph- 
ipoda of the Seto Inland Sea. II. Publ. Seto. Mar. Biol. 
Lab. 13: 171-186, figs. 16-26. 

Ricketts, E. F., & J. Calvin, 1968. Between Pacific Tides. 
4th edition. Stanford Univ. Press, California. 614 pp. 

Sars, G . O., 1895. Amphipoda. An account of the Crusta- 


cea of Norway. Christiana and Copenhagen. Vol 1. 
Amphipoda. pp. i-viii, 1-711, pis. 1-240, 8 suppl. pis. 

Savory, T., 1964. Arachnida. Academic Press, New York. 
291 pp., 109 figs. 

Shoemaker, C. R, 1952. A new species of commensal am- 
phipod from a spiny lobster. Proc.U. S. Natl. Mus. 102 
(3299): 231-233, 1 fig. 

, 1964. Seven new amphipods from the 

west coast of North America with notes on some unus- 
ual species. Proc. U.S. Natl. Mus. 115 (3489): 391-429. 

Sneath, P. H. A., & R. R. Sokal, 1973. Numerical Taxon- 
onomy. W. H. Freeman and Company, San Francisco. 
573 pp. 

Staude, C. P., 1987. Amphipoda: Suborder Gammaridea. 
pp. 346-391. in E. Kozloff (ed.). Marine Intertidal In- 
vertebrates of the Pacific Northwest. Univ. Washing- 
ton Press, Seattle. 51 1 pp. 

Stebbing, T. R. R., 1906. Amphipoda 1: Gammaridea. Das 
Tierreich, 21: 1-806. figs. 1-127. 

Tzvetkova, N. L., 1975. A new species of Pleustidae (Am- 
phipoda), a commensal of sea urchins, from the Kom- 
mander Islands. Zool. Zhum. 54:121-124, 1 fig. (in 
Russian). 

, & V. A. Kudrjaschov, 1985. On the fauna 

and ecology of gammarids (Amphipoda: Gammaridea) 
in the biocenosis of the upper parts of the shelf of South 
Sakhalin. Issled. Fauna Morei 20(38): 292-345, (in 
Russian). 

Watling, L., & D. Maurer, 1973. A new euryhaline species 
of Parapleustes (Amphipoda) from the east coast of 
North America. Proc. Biol. Soc. Wash. 86: 1-8, 4 figs. 

Wicksten, M. K., 1982. Cmstaceans from baited traps and 
gill nets off southern California. California Fish & Game 
68: 244-248, 1 fig. 


LEGEND FOR FIGURES 


A1 

antenna 1 

MX 1 - 

maxilla 1 

A2 

antenna 2 

MX2 - 

maxilla 2 

AC FL - 

accessory flagellum 


BR. 

coxal gill 

MXPD - 

maxilliped 

BR PL - 

brood plate 

O.P. - 

outer plate 

CX 

coxal plate(s) 

P3-P7 - 

peraeopods 3-7 

DACT - 

dactyl 

PLEOS - 

pleosome 

DORS - 

dorsal view 

PLP - 

palp 

EPl-3 - 

pleon plates 1-3 

RT 

right 

GNl 

gnathopod 1 

SET - 

seta(e) 

GN2 

gnathopod 2 

SP 

spine 

HD 

head 

T 

telson 

I.P. 

inner plate 

U1-U3 - 

uropods 1-3 

I.R. 

inner ramus 

UROS - 

urosome 

LFT 

left 

X 

magnified 

LL 

lower lip 

(f 

male 

MD 

mandible 

9 

female 


AMPHIPACIFICA VOL II NO. 1. AUG. 31, 1995 


134 


Additions to Amphipacifica, Voi. 1(4), 1995. 

The following catalogue numbers have been provided 
through the courtesy of the Invertebrate Curatorial Unit, 
Canadian Museum of Nature, Ottawa, pertinent to the 
following paper: 

Bousfield, E. L., & E. A. Hendrycks, 1995. The amphipod 
superfamily Eusiroidea in the North American Pacific Region. 

1. Family Eusiridae: systematics and distributional ecology. 
Amphipacifica I (4): 3-59. 

l .Eusiruscolumbianus Bousfield & Hendrycks, 1995, pp. 
10-11, fig. 5. 

Female (5.2 mm), Holotype (slide mount). CMN Cat. 
no. NMCC1995-0001. 

2. Rhachotropis calceolata Bousfield & Hendrycks, 1995, 
pp. 26-27, fig. 16. 

Female ov (8.7 mm), Holotype (slide mount). CMN 
Cat. no. NMCC1995-0005. 

3. Rhachotropis boreopacifica Bousfield & Hendrycks, 
1995, p. 29, fig. 17. 

Female br. I (10.5 mm), Holotype (slide mount). CMN 
Cat. no. NMCC 1995-0006. 

Female (unspecified), Paratype. CMN Cat. no. 
NMCC1995-0007. 

4. Rhachotropis minuta Bousfield & Hendrycks, 1995, p. 
35, fig. 22. 

Female ov (3.8 mm), Holotype (slide mount). CMN 
Cat. no. NMCC1995-0008. 

2 other females, ELB Stn. P3, West Bay, B. C., Nov. 2, 
1977, Paratypes. CMN Cat. no. NMCC 1995-0009. 


5. Rhachotropis conlanae Bousfield & Hendrycks, 1995, p. 
37, fig. 23. 

Female (4.5 mm), Holotype (slide mount). CMN Cat. 
no. NMCC1995-0010. 

Female (4. 1 mm), Bocade Quadra, southeastern Alaska, 
June 27, 1989, Paratype. CMN Cat. no. NMCC1995-001 1 . 

Catalogue numbers remain pending for the following 
species: 

1, Eusirus hirayamae Bousfield & Hendrycks, 1995, p. 10, 
fig. 3. 

Male (6.5 mm), Holotype. Ariake Sea, Japan. 

Original material described and figured (as E. longipes 
Boeck) in: Hirayama, A., 1985. Publ. Seto Mar. Biol. Lab. 
30; 29, figs. 142-147. Collections of the Amakusa Marine 
Biological Laboratory (AMBL), Amakusa, Japan. 

l.Cleonardomoirae Bousfield & Hendrycks, 1995, pp. 15- 
17, fig. 7. 

Female ov. (7.0 mm), Holotype. Institute of Ocean 
Sciences (lOS), Sidney, B. C. 

3. Rhachotropis barnardi Bousfield & Hendrycks, 1995, 
pp. 29-31, fig. 18. 

Male (3.3 mm), Holotype. Unspecified Paratypes. 
Original material briefly described and figured (as R. clemens 
Barnard) in; Barnard, J. L., 1971; Smiths. Contr. Zool. 61: 
10, figs. 6, 7. Off Oregon, 200 m. Collections of the United 
States National Museum, Washington, D. C. 

4. Rhachotropis americana Bousfield & Hendrycks, 1995, 
p. 40, fig. 26. 

Female (11.3 mm), Holotype (slide mount); male (9.5 
mm), AUotype); 5 females, 1 male, Paratypes. RBCM/ 
CMN Stn. 91-1-119. Collections of the CMN, Ottawa. 



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